Skip to main content

Full text of "Modern chemistry"

See other formats


THE  TEMPLE  PRIMERS 


MODERN   CHEMISTRY 
Systematic 

By 
WILLIAM  RAMSAY,  D.Sc. 


JOHN  DALTON 


mODERH 

CHEmiSTRY 

SYSTEI12ATN 


LAlttSAY'DS? 


1900*  ±9  &5O  BEDFORD-STREET* 


All  rights   reserved 


MODERN     CHEMISTRY 

SECOND    PART 
SYSTEMATIC  CHEMISTRY 

CHAPTER   I 

Methods  of  Preparing  Elements — Their  Physical 
Properties. 

Mixtures  and  Compounds. — In  the  olden  days,  no 
distinction  was  drawn  between  a  compound  and  a  mixture. 
Indeed,  all  "  impure  "  substances  artificially  prepared  were 
termed  "  mixts."  It  was  only  after  the  true  idea  of  ele- 
ments had  been  arrived  at,  and  indeed  not  until  Dalton  had 
formulated  the  laws  which  go  by  his  name,  that  the  distinc- 
tion was  drawn.  The  ultimate  criterion  for  combination  is 
definiteness  of  proportion,  and  this  is  generally  connected 
with  uniformity  in  properties,  or  homogeneity.  A  sub- 
stance is  said  to  be  homogeneous  when  no  one  part  of  it 
differs  from  any  other  part  in  composition.  But  this  may 
be  predicated  of  glass,  or  of  air,  which  are  mixtures,  and  not 
compounds.  A  mixture  may  be  homogeneous  ;  a  com- 
pound must. 

Again,  it  is  usually  accepted  that  the  separation  of  the 
constituents  of  a  mixture  may  be  effected  by  mechanical,  or 
at  least  by  physical  means  ;  whereas  the  separation  of  the 
elements  from  a  compound  require  chemical  treatment. 
Here  it  is  difficult  to  draw  a  sharp  distinction.  The 

VOL.   II.  A 

385213 


2  MODERN   CHEMISTRY 

separation  cf  carbon  dioxide  from  soda-water  by  the  appli-  . 
cation  of  heat  is  similar  in  character  to  the  separation  of 
sugar  from  water  by  evaporation  of  the  water  ;  yet  we 
believe  that  a  solution  of  carbon  dioxide  in  water  consti- 
tutes a  compound,  while  that  of  sugar  in  water  is  a  mere 
mixture  of  the  two.  It  is  necessary  to  be  guided  by  analogy 
in  the  former  case  ;  and  it  is  probable  that  the  compound 
named  carbonic  acid  is  really  contained  in  a  solution  of 
carbon  dioxide  in  water,  on  account  of  the  formulas  and 
behaviour  of  the  carbonates. 

The  Atmosphere. — In  the  case  of  mixtures  of  gases, 
the  problem  becomes  an  easier  one.  For  in  this  case,  each 
gas  retains  its  individual  properties.  The  atmosphere,  for 
example,  is  believed  to  be  a  mixture  of  the  gases 

Nitrogen,        .          .      78.16  per  cent. 
Oxygen,  .      20.90        „ 

Argon,  &c.,   .          .        0.94       „ 


100.00 


if  small  amounts  of  water-vapour,  of  carbon  dioxide,  and 
of  ammonia,  all  of  which  vary  considerably  in  amount,  be 
subtracted. 

This  can  be  shown  by  several  lines  of  argument. 

First,  The  density  of  air  agrees  with  the  mean  of  the 
densities  of  its  constituents,  taken  in  the  proportion  in  which 
they  occur.  Thus,  the  density  of  the  mixture  of  atmos- 
pheric nitrogen  and  argon  differs  by  only  I  part  in  40,000  from 
that  calculated  from  their  relative  weights,  and  the  proportion 
in  which  they  occur.  This  is  the  case  with  compound  gases 
only  when  the  constituents  are  present  in  equal  proportions 
by  volume,  as  in  hydrogen  chloride,  HC1.  The  above 
mixture  is  far  from  fulfilling  that  requirement. 

Second,  The  constituents  of  air  can  be  separated  by 
diffusion.  Thomas  Graham  discovered  that  the  rate  of 
escape  of  gases  through  an  opening,  or  of  passage  through 


THE  ATMOSPHERE  3 

a  porous  partition  is  inversely  in  the  order  of  the  square 
roots  of  their  relative  densities.  Now,  air  has  been  enriched 
in  oxygen  and  in  argon  by  diffusion  ;  the  lighter  nitrogen 

passes  more  rapidly  in  the  proportion  of 


—  /=  :      ,—  :  —7—, 
0/14     \/i6     V20 

the  last  two  fractions  referring  to  the  rates  of  oxygen  and 
argon  respectively  ;  the  oxygen  and  argon,  being  more  slowly 
diffusible,  are  left  to  the  last. 

Third,  The  constituents  of  air  may  be  separated  by 
solution  in  water.  While  oxygen  is  soluble  at  atmospheric 
temperature  in  the  proportion  of  about  3  volumes  in  100  of 
water,  nitrogen  is  much  less  soluble  —  about  1.5  volumes  ; 
and  argon  about  4.1  volumes*  Hence,  on  shaking  air  with 
water,  the  relative  volumes  dissolved  are  : 

Oxygen,  3  x  20.90  ;   Nitrogen,  1.5  x  78.16  ;   and 
Argon,  4.1  x  0.9  4, 

or  in  the  proportion  of  63  :  1  17  :  3.8.  It  is  evident 
that  the  relative  proportion  of  nitrogen  has  considerably 
decreased. 

Fourth,  The  elements  contained  in  air  are  not  present  in 
any  atomic  ratio.  To  ascertain  the  relative  number  of 
atoms  of  these  elements  it  is  necessary  to  divide  the  per- 
centage amount  of  each  by  its  atomic  weight  ;  thus  we  have 

Nitrogen,  Z_:   _  =  5.58  ;     Oxygen,   ^9  =  1.31  ; 

Argon,   2^51  =  0.024  ; 
40 

and  these  numbers  bear  to  each  other  no  simple  ratio. 

Lastly,  it  is  possible  by  distilling  liquid  air  to  separate 
the  more  volatile  nitrogen  from  the  less  volatile  oxygen 
and  argon. 

For  these  reasons,  and  other  similar  ones,  it  is  concluded 
that  air  is  a  mixture. 


4  MODERN   CHEMISTRY 

The  Analysis  of  the  Atmosphere  is,  however, 
always  performed  by  chemical  means,  for  the  difference  in 
physical  properties  of  its  constituents  is  not  sufficiently 
marked  to  allow  of  their  being  utilised  for  purposes  of 
separation.  Many  common  elements  unite  easily  with 
oxygen  to  form  non-volatile  compounds,  when  they  are 
heated  in  air.  One  of  the  most  convenient  for  this 
purpose  is  metallic  copper.  By  passing  a  known  volume 
of  air  over  copper  turnings,  contained  in  a  counter- 
poised tube  of  hard  glass,  and  heated  to  redness,  the 
oxygen  of  the  air  is  removed,  for  it  combines  with  the 
copper  to  form  non- volatile  black  oxide  of  copper.  The  in- 
crease in  weight  of  this  tube  gives  the  weight  of  the  oxygen  in 
the  measured  volume  of  air.  But  it  is  customary  to  analyse 
air  volumetrically  by  absorbing  the  oxygen  from  a  known 
volume  by  means  of  burning  phosphorus,  or  of  a  solution  of 
potassium  pyrogallate  :  the  remainder  consists  of  a  mixture  of 
nitrogen,  argon  and  its  congeners.  The  separation  of  these 
gases  from  each  other  is  described  in  the  next  paragraph. 

Reference  has  already  been  made  in  Part  I.  to  the  different 
processes  which  may  be  used  for  the  isolation  of  elements 
from  their  compounds.  But  there  exists  a  group  of  elements, 
that  of  which  the  first  member  is  helium,  which  form  no  com- 
pounds, and  which  therefore  are  found  only  in  a  free  state. 
It  is,  therefore,  convenient  to  begin  with  these. 

The  HELIUM  Group. — These  elements  are  all  gases  at 
the  ordinary  temperature  of  the  atmosphere,  and  they  are 
consequently  all  to  be  found  in  atmospheric  air.  They  are 
colourless,  even  in  the  liquid  condition,  and  are  devoid  of 
smell  and  taste.  They  are  very  sparingly  soluble  in  water ; 
for  example,  100  volumes  of  water  dissolve  only  4.1  volumes 
of  argon  at  1 5°.  Their  preparation  consists,  first,  in  the 
separation  of  the  other  constituents  of  air  from  them,  and, 
second,  in  their  separation  from  each  other. 

Air,  which  is  a  mixture,  and  not  a  compound,  of  nitro- 
gen, oxygen,  carbon  dioxide,  ammonia,  water-vapour,  and 
the  gases  of  the  helium  group,  is  a  supporter  of  combustion, 


THE   HELIUM   GROUP  5 

owing  to  the  combination  of  the  oxygen  which  it  contains 
with  most  other  elements.  Now,  when  air  passed  through 
a  tube  full  of  a  mixture  of  caustic  soda  and  lime,  to  remove 
carbon  dioxide,  and  then  through  a  U-tube  containing  sul- 
phuric acid,  to  deprive  it  of  water-vapour  and  ammonia,  is  led 
over  red-hot  copper,  or  over  some  other  red-hot  metal  which 
unites  with  oxygen,  the  oxygen  is  retained,  and  nitrogen  with 
members  of  the  helium  group  alone  passes  on.  The  nitrogen 
can  be  removed  in  one  of  two  ways.  The  first  plan  is  due 
to  Cavendish,  who  attempted  to  prove  that  atmospheric  nitro- 
gen was  a  homogeneous  substance.  He  mixed  atmospheric 
nitrogen  with  oxygen,  and  passed  electric  sparks  through 
the  mixture,  having  a  little  caustic  soda  present  in  the 
tube.  Under  the  influence  of  the  sparks,  the  nitrogen  and 
oxygen  combine,  giving  nitride  peroxide,  NO9  ;  this  com- 
pound is  absorbed  by  the  soda,  with  formation  of  sodium 
nitrate  and  nitrite,  NaNO3  and  NaNO2.  Cavendish 
obtained  a  residue  of  not  more  than  one-hundred-and- 
twentieth  of  the  nitrogen ;  and  he  concluded  that  if 
atmospheric  nitrogen  was  not  homogeneous,  it  contained  only 
a  trace  of  another  gas.  The  second  plan  is  to  pass  the 
atmospheric  nitrogen  over  red-hot  magnesium,  or,  better,  over 
a  mixture  of  magnesium  powder  and  lime,  which  gives 
calcium  ;  the  magnesium  or  the  calcium  unites  with  the 
nitrogen,  and  the  inert  gases  pass  on. 

To  separate  these  gases  from  each  other,  they  are 
compressed  into  a  bulb,  cooled  to  -185°  by  being  immersed 
in  liquid  air.  The  argon,  krypton,  and  xenon  condense  to 
a  liquid,  in  which  the  neon  and  helium  are  dissolved.  On 
removing  the  bulb  from  the  liquid  air,  its  temperature  rises, 
and  the  helium  and  neon  escape  first,  mixed  with  a  large 
amount  of  argon.  Argon  distils  next,  and  krypton  and  xenon 
remain  till  the  last.  By  frequently  repeating  this  process 
of  "  fractional  distillation,"  the  argon,  krypton,  and  xenon 
can  be  separated  from  each  other,  and  from  the  helium  and 
neon  which  still  remain  mixed  with  each  other,  for  both 
are  gases  at  the  temperature  of  boiling  air. 


6  MODERN   CHEMISTRY 

To  separate  helium  from  neon,  recourse  must  be  had  to 
liquid  hydrogen.  To  liquefy  hydrogen,  the  process  is  in 
principle  the  same  as  that  for  liquefying  air,  described  on 
p.  26.  The  hydrogen,  compressed  by  a  pressure  of  200 
atmospheres,  is  cooled  to  —205°  by  passing  through  a  coil  of 
copper  pipe,  immersed  in  liquid  air  boiling  under  low 
pressure.  On  expanding,  its  temperature  is  still  further 
lowered,  and  the  still  colder  gas,  in  passing  upwards,  cools 
the  tubes  through  which  the  compressed  gas  is  passing. 
The  hydrogen  finally  issues  in  the  liquid  state,  as  a  colour- 
less, mobile  liquid,  of  the  approximate  temperature  —240°. 
By  its  aid,  if  a  mixture  of  neon  and  helium  is  cooled  to 
—240°,  the  former  freezes,  while  the  latter  remains 
gaseous.  The  gaseous  helium  can  be  removed  with  the 
pump  ;  and  the  neon,  after  it  has  been  warmed,  may  also  be 
pumped  off  in  a  pure  state. 

Helium  can  also  be  prepared  by  heating  certain  specimens 
of  pitchblende  or  uraninite,  a  mineral  consisting  chiefly  of 
oxide  of  uranium.  The  gas,  which  appears  to  exist  in  some 
sort  of  combination  with  the  uranium  oxide,  escapes  ;  it 
contains  a  trace  of  argon.  All  these  gases  give  very  striking 
spectra,  and  that  of  helium  was  observed  during  the  solar 
eclipse  of  1 868  in  the  chromosphere,  or  coloured  atmosphere, 
of  the  sun.  Although  at  that  time  it  had  not  been  dis- 
covered on  the  earth,  the  name  "  helium  "  was  given  to 
the  bright  yellow  line,  which  is  the  most  characteristic  of 
its  spectrum. 

As  regards  the  relative  amount  of  these  gases  contained 
in  air,  100  volumes  of  air  contain  0.937  volume  of  the 
mixture.  By  far  the  largest  portion  of  this  mixture  is 
argon  ;  probably  the  volume  of  all  the  others  taken  together 
does  not  exceed  one-four-hundredth  part  of  that  of  the 
argon.  Indeed,  it  may  be  said  with  truth  that  there  is  less 
xenon  in  air  than  there  is  gold  in  sea-water. 

Methods  of  Separating  Elements  from  their 
Compounds* — The  methods  of  preparation  of  the  remain- 
ing elements  depend  on  considerations  of  the  cost  of  the 


SEPARATION   PROCESSES  7 

compound  from  which  the  element  is  to  be  prepared,  and  on 
the  ease  of  preparation.  In  the  case  of  those  elements  which 
are  required  on  a  commercial  scale,  like  iron,  for  example, 
the  process  of  manufacture  is  regulated  chiefly  by  the  cost 
of  the  ore,  and  of  the  operations  necessary  to  produce  the 
metal  in  a  state  of  purity  sufficient  for  commercial  purposes. 
But  if  perfectly  pure  iron  is  required  for  scientific  purposes — 
for  example,  in  order  to  determine  its  electrical  properties — 
then  the  question  of  cost  does  not  come  into  consideration, 
and  processes  are  adopted  which  are  necessarily  very  costly. 
In  the  description  which  follows,  however,  we  shall  give 
only  the  ordinary  methods  of  preparation. 

Again,  the  process  chosen  depends  greatly  on  the  physical 
and  chemical  properties  of  the  element  which  it  is  desired  to 
isolate.  Some  elements  are  volatile,  and  are  more  or  less 
easily  separated  by  distillation  from  the  material  from  which 
they  are  produced  ;  some  elements  are  attacked  by  water, 
while  others  resist  attack  ;  some  fuse  at  comparatively  low 
temperatures,  and  can  thus  be  separated,  while  others  are 
producible  in  a  compact  state  only  at  the  enormously  high 
temperature  of  the  electric  arc.  It  is  necessary,  therefore,  to 
know  the  properties  of  the  element  required  before  deciding 
on  a  process  for  its  isolation.  The  preparation  of  the 
remaining  elements  will  therefore  be  considered  from  this 
point  of  view. 

( i )  Separation  of  the  element  by  means  of  an 
electric  current. 

(a)  From  a  fused  salt. — One  condition  is  that  the 
salt  shall  fuse  at  a  convenient  temperature — that  is,  at  or 
below  a  red  heat.  Another  is  that,  in  the  case  of  metals 
which  are  commercially  used,  the  salts  must  be  cheaply 
obtainable,  and  the  metals  easily  separated  from  the  salts. 

It  is  interesting  to  note  that  this  process  led,  in  the  hands 
of  Sir  Humphry  Davy,  to  the  discovery  of  the  metals 
of  the  alkalies,  potassium  and  sodium ;  he  first  prepared 
them  by  passing  a  current  from  a  battery  of  high  voltage 


8  MODERN   CHEMISTRY 

through  the  hydroxide,  melted  on  a  piece  of  platinum  foil. 
The  metal  was  visible  only  for  an  instant ;  for  it  floated 
up  from  the  electrode  of  platinum  wire,  and  burst  into 
flame  as  soon  as  it  came  into  the  air. 

As  a  rule,  however,  the  chlorides  are  the  most  con- 
venient salts  for  electrolysis.  From  the  known  fact  that 
the  melting-point  of  a  compound  is  lowered  by  the  presence 
of  an  "impurity,"  it  is  often  found  advantageous  to  electro- 
lyse a  mixture  of  chlorides  rather  than  a  pure  chloride  ; 
in  this  case  one  of  the  elements  is  liberated  in  preference 
to  the  other.  As  the  anode  has  to  withstand  the  action 
of  chlorine,  it  is  always  made  of  carbon,  which  does  not 
unite  with  chlorine  directly ;  the  kathode  may  be  of  iron, 
a  metal  which  has  no  tendency  to  form  alloys  with  those 
which  are  prepared  in  this  way,  at  least  at  the  temperatures 
required.  The  kathode  may  be  the  iron  pot  in  which  the 
chloride  is  kept  fused. 

The  elements  which  are  prepared  in  this  way  are : 
lithium,  sodium,  potassium,  rubidium,  caesium,  beryllium, 
magnesium,  calcium,  strontium,  and  barium.  The  first  five 
are  easily  fusible  white  soft  metals,  which  take  fire  when 
heated  in  air,  and  must  therefore  be  kept  in  an  atmosphere 
free  from  oxygen ;  they  also  attack  water, liberating  hydrogen, 
with  formation  of  the  hydroxide  MOH.  Their  density 
is  so  low  that  they  float  on  their  fused  chlorides ;  they 
must,  therefore,  be  liberated  in  the  interior  of  a  bell-shaped 
iron  electrode  or  of  a  fireclay  receptacle,  down  which  an 
iron  kathode  passes.  Beryllium  and  magnesium  are  better 
prepared  from  a  mixture  of  their  chlorides  with  potassium 
chloride ;  the  latter  melts  and  collects  at  the  bottom  of  the 
pot,  which,  in  this  case,  may  be  the  kathode.  They  are 
hard  white  metals,  magnesium  melting  at  about  750°,  and 
beryllium  about  1 200°.  They,  too,  take  fire  when  heated 
in  air,  and  burn  with  a  brilliant  flame ;  indeed,  the  chief 
use  of  magnesium  is  for  signalling  purposes.  The  metal  is 
drawn,  while  hot,  into  wire,  which  is  then  rolled  into 
ribbon;  this  ribbon  burns  with  an  exceedingly  bright  flame, 


METALS   OF  THE  ALKALIES  9 

producing  the  oxide  MgO.  Calcium,  strontium,  and 
barium  are  also  white  metals ;  they  have  been  produced  by 
electrolysis  of  their  cyanides,  M(CN)2,  compounds  which 
fuse  at  a  lower  temperature  than  the  chlorides.  They  are 
very  readily  attacked  by  water,  yielding  the  hydroxides 
M(OH)0.  The  only  two  of  these  metals  which  find 
commercial  use  are  sodium  and  magnesium. 

Aluminium,  which  is  also  manufactured  on  a  large  scale, 
is  produced  from  its  ore,  bauxite,  from  which  pure  alumina, 
the  oxide,  is  first  prepared.  The  alumina  is  dissolved  in 
fused  cryolite,  a  fluoride  of  aluminium  and  sodium  of  the 
formula  NagAlF6,  deposits  of  which  occur  in  Greenland. 
The  aluminium  sinks  to  the  bottom  of  the  crucible,  and 
when  a  sufficient  quantity  accumulates  it  is  tapped  out. 
The  "flux,"  as  the  cryolite  is  termed,  is  again  melted, 
and  a  further  quantity  of  alumina  is  dissolved  in  it.  The 
metal  is  fairly  hard,  white,  susceptible  of  a  high  polish, 
ductile  and  malleable.  It  is  also  very  light  (about  two  and 
a  half  times  as  heavy  as  water),  and  not  easily  oxidised  in  air 
at  the  ordinary  temperature,  nor  is  it  attacked  by  water. 

(b)  From  a  dissolved  salt. — Gallium,  a  tin- white, 
hard  metal,  very  rare,  contained  in  some  zinc  ores,  is 
deposited  from  a  solution  of  its  hydroxide  in  caustic 
potash.  Copper  prepared,  as  will  be  seen  below,  in  a 
crude  state  by  displacement,  is  purified  by  electrolysis. 
It  is  of  the  utmost  importance  to  employ  pure  copper  for 
the  conduction  of  electric  currents  ;  for  although  copper 
is  one  of  the  best  conductors,  its  resistance  is  enormously 
increased  by  the  presence  of  a  very  small  trace  of  impurity. 
To  purify  it,  large  rectangular  blocks  of  crude  copper  are 
suspended  close  to  thin  sheets  of  pure  copper  in  an  acid 
bath  of  copper  sulphate,  CuSO4.Aq.  The  heavy  block 
is  made  the  anode  and  the  thin  sheet  the  cathode;  the 

sulphation,    SO4,    in    discharging    at    the    anode,    dissolves 
copper  from  the  thick  block  as  sulphate;   while  the  cuprion, 
+  + 
Cu,  in  yielding  up  its  charge  at  the  kathode,  deposits  on 


TO  MODERN   CHEMISTRY 

the  latter  and  increases  its  thickness.  The  impurities, 
arsenic,  antimony,  and  iron,  remain  in  solution,  and  a 
sludge  is  deposited  containing  silver  and  gold,  besides 
traces  of  many  other  elements.  Copper  is  a  very  malleable, 
ductile  red  metal,  melting  at  1330°. 

Objects  of  iron  are  often  "  nickel-plated,"  or  covered 
with  a  thin  film  of  nickel,  a  white,  hard  metal  which  pre- 
serves its  lustre  in  air,  for  it  is  not  easily  oxidisable.  This  is 
done  by  making  the  object  to  be  coated  with  nickel  the  kathode 
and  a  bar  of  nickel  the  anode ;  the  liquid  is  a  solution 
of  oxalate  of  nickel  and  potassium.  Iron  objects  are  first 
coated  with  copper  before  nickelling.  Silver  and  gold  are 
best  deposited  from  their  double  cyanides  with  potassium  ; 
these  salts  are  used  because  the  deposit  is  harder  and  more 
uniform  than  if  a  halide  be  used.  In  thus  coating  objects, 
it  is  of  importance  that  the  current  density,  i.e.  the  ratio 
of  the  current  to  the  area  of  the  surface  of  the  object  to  be 
coated,  should  be  considered  ;  if  this  be  too  high,  the  metal 
will  be  deposited  in  a  loose,  flocculent  condition. 

As  an  illustration  of  the  changes  which  take  place  during 
such  electrolysis,  the  deposition  of  silver  may  be  chosen. 
The  compound  employed  is,  as  stated,  the  double  cyanide 
(see  p.  187)  ;  its  formula  is  KAg(CN)2,  and  the  ions 

+ 
are  K  and  Ag(CN)2.      There  are,  however,  at  the  same 

+ 

time  a  few  ions  of  Ag  and  CN.  From  the  last,  metallic 
silver  is  deposited  on  the  kathode ;  and  as  soon  as  its 
amount  is  reduced,  a  fresh  quantity  is  formed  by  the 

decomposition  of  the  complex  ion,  Ag(CN)9.  The 
formation  and  deposition  of  the  silver  ion  goes  on  con- 
tinuously until  all  the  silver  required  has  been  deposited. 
Similar  changes  take  place  during  the  electro-deposition  of 
nickel  and  of  gold. 

Modern  electrolytic  processes  for  obtaining  chlorine  and 
caustic  soda  (NaOH)  from  salt  result  in  the  liberation  of 
enormous  quantities  of  hydrogen.  The  salt,  dissolved  in 


ELECTRO-DEPOSITION  11 

water,  is  placed  in  a  tank  divided  into  two  compartments 
by  a  porous  diaphragm  ;  the  anode,  which  consists  of 
carbon  rods,  dips  into  one,  and  the  kathode,  which  may 
be  formed  of  copper  plates,  in  the  other.  The  ions,  of 

+ 

course,  are  Na.Aq,  and  Cl.Aq.  The  chlorine  is  liber- 
ated at  the  anode,  and  the  sodium  at  the  kathode.  But  as 
soon  as  the  sodion  is  discharged,  it  reacts  with  the  water, 
forming  caustic  soda,  thus  :  2Na  +  2HOH  =  aNaOH  +  H2. 
Hence  the  production  of  hydrogen.  Bromine  and  iodine 
may  be  liberated  in  the  same  way  as  chlorine,  the  bromide 
or  iodide  of  sodium  or  potassium  being  substituted  for  the 
chloride.  As  fluorine  at  once  acts  on  water,  liberating 
•  oxygen  in  the  form  of  ozone,  O3,  it  cannot  be  produced 
from  an  aqueous  solution  of  a  fluoride  ;  but  it  has  been  found 
that  liquid  hydrogen  fluoride  has  ionising  power,  so  that  on 
passing  a  current  between  poles  of  platinum-iridium  (an 
alloy  of  metals  which  is  less  attacked  by  fluorine  than  any 
other  conductor)  through  a  solution  of  hydrogen-potas- 
sium fluoride,  HKF,  in  pure  liquid  hydrogen  fluoride, 
H^F^,  at  -30°,  fluorine  is  evolved  from  the  anode 
as  a  pale  yellow  gas  with  a  strong  characteristic  smell, 
somewhat  resembling  that  of  the  other  halogens,  chlorine, 
bromine,  and  iodine ;  while  hydrogen  is  evolved  at  the 
kathode,  having  been  produced  by  the  action  of  the  potas- 
sium on  the  hydrogen  fluoride.  Fluorine  boils  at  —195°, 
chlorine  at  -35°,  bromine  at  59°,  and  iodine,  which  is  a 
solid  at  atmospheric  temperature,  melts  at  114°  and  boils 
at  184°.  The  colours  of  these  elements  also  show  a 
gradation.  Chlorine  is  greenish-yellow;  bromine,  red  both 
as  gas  and  liquid ;  iodine  is  a  blue-black  solid  and  a  violet 
gas.  These  three  elements  are  somewhat  soluble  in  water, 
and  more  so  in  a  solution  of  their  soluble  salts.  It  has 
recently  been  found  that  another  ionising  agent  than  water 
may  be  used.  Lithium  chloride  is  soluble  in  pyridine,  a 
compound  of  the  formula  C5H5N,  and  may  be  electro- 
deposited  on  a  platinum  kathode  from  such  a  solution. 


12  MODERN   CHEMISTRY 

The    metal    is    not    attacked    by   pyridine ;    the    chlorine, 
however,  is  rapidly  absorbed. 

(2)  Separation  of  an  element  from  a  compound 
"by  rise  of  temperature. 

This  method  is  applied  in  practice  only  to  the  prepara- 
tion of  oxygen,  and  of  chlorine,  bromine,  and  iodine ;  but 
many  other  elements  may  be  thus  made,  where  the  com- 
pound heated  does  not  tend  to  re-form  on  cooling.  These 
cases  will  be  considered  first. 

Ordinary  coal-gas  consists  chiefly  of  methane,  CH4, 
ethylene,  C2H4,  carbon  monoxide,  CO,  and  hydrogen, 
the  last  amounting  to  nearly  50  per  cent,  of  the  volume 
of  the  gas.  This  hydrogen  owes  its  origin,  at  least  in 
part,  to  the  decomposition  of  its  compounds  with  carbon, 
by  their  coming  into  contact  with  the  red-hot  walls  of  the 
retort  in  which  the  coal  is  distilled.  Carbon  deposits  in  a 
dense  black  mass  on  the  iron,  and  is  removed  from  time  to 
time  with  a  chisel.  Hydrogen  escapes  and  mixes  with  the 
coal-gas.  This  form  of  carbon  is  used  for  the  pencils  for 
arc-lights,  and  for  the  anodes  of  Bunsen's  and  other  forms  of 
cells,  and  also  for  anodes  in  electro-chemical  processes. 

The  compounds  of  hydrogen  with  nitrogen  (ammonia, 
NH3),  sulphur,  selenium,  and  tellurium  (sulphuretted, 
seleniuretted,  or  telluretted  hydrogen,  H9S,  H2Se,  H0Te), 
all  of  which  are  gases  at  the  ordinary  temperature,  are  de- 
composed if  passed  through  a  red-hot  tube,  giving  hydrogen, 
which  escapes  along  with  nitrogen  if  ammonia  be  heated ; 
or  a  deposit  of  the  sulphur,  &c.,  in  the  cold  part  of  the  tube 
if  one  of  the  other  gases  mentioned  be  employed. 

The  oxides  of  the  metals  ruthenium,  rhodium,  palladium, 
silver,  osmium,  iridium,  platinum,  gold,  and  mercury  are 
decomposed  at  a  red  heat ;  and  the  chlorides,  bromides, 
iodides,  and  sulphides  are  also  decomposed,  except  those 
of  silver  and  mercury. 

But  none  of  these  methods  are  practical  plans  of  prepar- 
ing the  elements.  On  the  other  hand,  as  already  stated, 


DECOMPOSITION    BY  HEATING  13 

this  method  is  generally  used  for  the  production  of  oxygen. 
This  gas,  although  it  had  probably  been  obtained  in  an 
impure  state  by  the  older  experimenters,  was  first  pro- 
duced in  approximate  purity  by  Priestley  and  simul- 
taneously by  Scheele  in  1774.  Priestley  produced  it  by 
heating  mercuric  oxide,  HgO,  which  decomposes  thus : 
2HgO  =  2Hg  +  O2.  And  Lavoisier  showed  that  it  was 
possible  to  produce  mercuric  oxide  by  heating  mercury  to 
its  boiling-point  in  a  confined  portion  of  air,  and  by  sepa- 
rating and  weighing  the  oxide,  and  subsequently  heating  it 
till  it  decomposed  again,  he  proved  that  the  oxygen  had 
really  been  extracted  from  the  air. 

Certain  oxides  are  not  wholly  decomposed  into  oxygen 
and  element  when  heated,  but  leave  an  oxide  containing 
less  oxygen  than  that  originally  heated.  Among  these  is 
black  manganese  dioxide,  a  mineral  named  pyrolusite ; 
3MnO2  =  Mn3O4  +  O0.  Lead  dioxide  undergoes  a  similar 
change:  2PbO9=  zPbO  +  O9.  The  most  important  ap- 
plication of  this  method,  however,  is  the  commercial  plan 
of  producing  oxygen  carried  out  in  the  "  Brin  Company's  " 
works.  In  their  process,  barium  oxide,  BaO,  is  heated 
in  iron  tubes  under  pressure,  air  being  pumped  in.  The 
barium  oxide  absorbs  the  oxygen  of  the  air,  the  nitrogen 
being  allowed  to  escape.  After  the  operation  has  gone  on 
for  about  five  minutes,  a  considerable  amount  of  oxygen  is 
absorbed,  barium  dioxide,  BaO2,  being  formed.  The 
stopcocks  of  the  pipes  leading  to  the  pump  are  then 
reversed,  so  that  gas  is  exhausted  from  the  hot  iron 
tubes.  When  the  pressure  is  reduced,  the  barium  dioxide 
loses  oxygen,  and  again  returns  to  the  state  of  monoxide : 
2BaO2  =  2 BaO  +  O2.  The  pumping  is  continued  for  about 
five  minutes,  and  the  valves  are  again  reversed.  The  pro- 
cess is  thus  a  continuous  one  ;  the  oxygen  is  not  pure,  for 
it  contains  about  7  per  cent,  of  nitrogen  ;  but  for  medical 
use  in  cases  of  pneumonia,  and  for  the  oxy-hydrogen  blow- 
pipe, its  purity  is  sufficient. 

This  method  of  preparing  oxygen  is  an  instance  of  what 


I4  MODERN   CHEMISTRY 

is  termed  "  mass-action."  The  temperature  is  kept  con- 
stant, but  the  pressure  is  raised  when  it  is  desired  to  cause 
the  oxide  to  absorb  oxygen,  and  lowered  when  it  is  neces- 
sary to  remove  the  oxygen.  When  pressure  is  raised,  the 
number  of  molecules  of  oxygen  in  unit  volume  of  the  space 
ifor  the  mass)  is  increased,  and  hence  the  number  in  contact 
with  the  absorbing  medium,  the  barium  oxide.  Combina- 
tion, therefore,  takes  place  between  the  two.  On  reducing 
pressure,  the  number  per  unit  volume  is  reduced,  and  the 
compound  decomposes.  The  phenomenon  is  analogous 
with  the  behaviour  of  a  vapour  when  it  is  compressed ; 
after  a  certain  pressure  has  been  reached — the  vapour 
pressure — the  vapour  condenses  to  a  liquid,  and  if  more 
vapour  be  compressed  into  the  same  space,  the  pressure 
does  not  rise  further,  but  more  vapour  is  condensed :  this 
is  analogous  to  the  formation  of  more  BaO2.  On  pumping 
out  vapour,  the  pressure  does  not  fall,  but  the  liquid 
evaporates :  this  is  the  analogue  of  the  decomposition  of 
the  BaO2  into  BaO.  The  law  of  mass-action  is  very 
generally  applicable. 

Certain  oxides,  for  instance,  pentoxide  of  iodine,  I2O5, 
and  of  nitrogen,  N0O5,  decompose  when  heated.  These 
oxides  form  combinations  with  the  oxides  of  many  other  ele- 
ments, such  as  sodium  or  potassium  oxide,  e.g.  Na2O.I2O5 
or  NaIO3,  K2O.N2O5  or  KNO3 ;  a  similar  compound  is 
potassium  chlorate,  KClOg  or  K^O-C^O^  although  the 
simple  oxide  of  chlorine  is  unknown.  Now,  potassium 
and  sodium  oxides  are  not  decomposed  by  heat,  and  when 
these  salts  are  heated  oxygen  is  evolved  from  the  pentoxide 
of  chlorine  or  iodine.  These  elements,  however,  do  not 
escape,  but  replace  the  oxygen  combined  with  the  sodium 
or  potassium,  forming  chloride  of  the  metal,  thus : 
K2O.C12O5  =  K2O+  C12  +50,  and  K2O  +  CJ2=2KC1 
+  O,  or,  summing  up  both  changes  in  one  equation,  2KC1O3 
=  2KC1  +  3O2.  Nitrate  of  potassium,  on  the  other  hand, 
loses  only  one  atom  of  oxygen,  leaving  nitrite: 


DECOMPOSITION    BY   HEATING  15 

Oxygen  is  a  colourless  gas,  without  smell  or  taste  ;  it 
can  be  liquefied,  at  a  high  pressure  and  a*  low  temperature, 
to  a  pale  blue  liquid  boiling  at  —182°.  Most  elements 
unite  directly  with  it,  often  with  such  a  rise  of  temperature 
that  incandescence  is  produced  ;  in  such  a  case  the  pheno- 
menon is  termed  "combustion/'  In  many  instances,  for 
example  when  iron  rusts,  the  oxidation  is  not  attended  by 
any  measurable  rise  of  temperature,  although;  in  all  cases 
heat  is  evolved,  but  in  some  cases  extremely  slowly. 

Chlorine,  bromine,  and  iodine  are  generally  prepared  by 
heating  together  a  chloride,  bromide,  or  iodide  with  man- 
ganese dioxide  an^  sulphuric  acid  diluted  with  water. 
Here  the  first  change  is  the  formation  of  the  halogen 
hydride,  HC1,  HBr,  or  HI.  The  hydride,  however,  is 

+  - 

ionised  in  water,  and  the  HCl.Aq.,  for  example,  at  once 
reacts    with    the    MnO9,   forming    non-ionised   water    and 


MnCl4.  Aq,  thus  :  MnO2  +  4HC1.  Aq.  -  M  n  C  14.  Aq.  + 
2H>7O.  Tetrad  manganese,  however,  appears  not  to  be  able 
to  co-exist  with  chlorine  in  solution  ;  hence  the  manganese 


loses  an  electron  and  becomes  Mn,  the  lost  charge  neutralis- 
ing one  of  the  charged  chlorine  ions,  which  escapes  in  an 


electrically  neutral  state.  Even  then,,  however,  the  Mn, 
though  capable  of  existence  at  low  temperature,  still  loses 
a  charge,  and  a  second  chlorine  atom  is  liberated  in  a  non- 

ionised  state.     Hence  the  whole  change  is:  Mn     Cl4.Aq. 

+  +    - 

=  MnCl2.Aq.  +  C12.  Summing  all  these  changes  in  one 
equation,  we  have:  MnO2  +  zNaCl.Aq.  +  2H2SO4.Aq. 
-  MnSO4.  Aq.  +  Na2SO4.  Aq.  +  2H2O  +  C12  ;  or,  if  hydro- 
chloric acid  alone  be  warmed  with  manganese  dioxide, 
MnO2  +  4HC1.  Aq.  «  MnCl.,.  Aq.  +  2H2O  +  C12. 

(  3  )  Separation  of  an  element  from  a  compound  by 
displacement.  —  This  is  by  far  the  most  general  method 


16  MODERN   CHEMISTRY 

of  preparing  elements.  The  elements  commonly  used  as 
displacing  agents  are  : — 

(a)  Hydrogen  at  a  red  heat. — The  oxide  or  chloride 
is  placed  in  a  tube  of  hard  glass,  heated  to  600°  or  700° 
in  a  tube-furnace,  and  a  stream  of  dry  hydrogen  is  passed 
through  the  tube.  Water  or  hydrogen  chloride  is  formed, 
and  is  carried  on  by  the  current  of  hydrogen,  and  the 
element  i-s  left.  Indium,  thallium,  germanium,  tin,  lead, 
antimony,  and  bismuth  are  left  in  fused  globules,  solidifying 
to  white  lustrous  metallic  beads  ;  arsenic  gasifies  and  con- 
denses in  the  unheated  part  of  the  tube  as  a  grey  deposit ; 
tellurium,  which  is  also  volatile,  condenses  as  a  lustrous 
metallic  solid ;  while  iron,  cobalt,  nickel,  copper,  and  silver 
do  not  fuse  at  that  temperature.  The  first  three  remain  as 
grey  powders,  the  copper  as  a  red  powder,  and  the  silver 
in  a  white  spongy  condition.  These  metals  can  be  fused 
by  heating  them  in  a  crucible  to  a  sufficiently  high  tem- 
perature ;  it  is  well  to  use  a  "  flux,"  or  substance  to  make 
them  flow,  such  as  sodium  carbonate  or  borax  ;  the  flux 
fuses,  and  dissolves  any  film  of  oxide  off  the  surface  of  the 
metallic  beads,  and  they  then  join  up  to  form  a  single  mass 
of  molten  metal. 

(1}  Displacement  by  means  of  sodium  at  a  red 
heat. — The  chlorides  of  beryllium,  magnesium,  calcium, 
strontium,  barium,  aluminium,  scandium,  yttrium,  lantha- 
num, ytterbium,  cerium,  thorium,  vanadium,  niobium,  and 
tantalum  are  all  reduced  when  added  to  sodium  kept  melted 
in  an  iron  crucible.  For  boron,  silicon,  and  titanium  the 
double  fluoride  is  more  convenient,  for  the  chlorides  are 
volatile  liquids.  The  process  for  manufacturing  magne- 
sium, which  is  carried  out  on  a  large  scale,  may  be  more 
minutely  described  as  an  example.  The  double  chloride 
of  magnesium  and  potassium,  MgCl2.KCl,  carefully  dried, 
is  mixed  with  sodium  in  proportion  to  unite  with  the 
chlorine  of  the  MgCl2,  the  sodium  being  in  small  lumps. 
The  iron  crucible  containing  the  mixture  is  heated ;  a 
violent  reaction  takes  place,  and  magnesium  is  liberated : 


DISPLACEMENT  17 

MgCl.2.  KC1  +  2Na  -  Mg  +  zNaCl  +  KC1.  As  magnesium 
is  volatile,  and  can  be  distilled,  it  is  purified  by  this 
operation.  The  contents  of  the  crucible  are  treated  with 
water ;  the  potassium  and  sodium  chlorides  dissolve,  and 
the  globules  of  magnesium  are  collected,  dried,  and  placed 
in  a  crucible,  through  the  bottom  of  which  a  tube  is  fixed 
reaching  nearly  to  the  lid,  and  projecting  some  distance 
below  the  bottom.  This  crucible  is  placed  in  a  furnace, 
and  on  raising  the  temperature,  the  magnesium  volatilises 
up,  passes  down  the  tube,  and  the  vapour  condenses  in  the 
cooler  part  of  the  tube  which  projects  below  the  furnace. 
This  particular  method  of  distillation  is  called  destillatio  per 
descensum.  The  other  elements  mentioned  are  too  little 
volatile  to  admit  of  purification  by  this  means.  In  their 
case,  the  cooled  mass  is  treated  with  alcohol  in  order  to 
remove  the  excess  of  sodium,  and  then  with  water  to 
dissolve  the  resulting  salt ;  the  element  is  left  in  the  state 
of  powder. 

(c)  Displacement  by  means  of  magnesium  at  a  red 
heat — This  process  is  sometimes  used  to  prepare  the 
element  from  its  oxide.  A  mixture  is  made  of  magnesium 
filings  with  the  oxide  of  the  element,  and  it  is  heated  in  an 
iron  crucible.  The  resulting  mass  is  then  treated  with 
hydrochloric  acid  to  remove  the  oxide  of  magnesium,  which 
is  thus  converted  into  the  soluble  chloride.  It  is,  of  course, 
essential  that  the  liberated  element  shall  not  be  attacked  by 
hydrochloric  acid.  The  process  works  for  the  preparation 
of  boron,  silicon,  and  titanium. 

(</)  Displacement  by  heating  the  oxide  with  car- 
bon.— This  process  is  of  the  most  general  application.  If 
the  element  is  volatile,  it  is  distilled  from  an  iron  or  fire- 
clay retort ;  in  this  way  sodium,  potassium,  rubidium, 
arsenic,  zinc,  and  cadmium  are  prepared.  If  non-volatile 
at  a  red  heat,  a  mixture  of  the  oxide  with  charcoal  is 
heated  to  bright  redness  in  a  clay  crucible.  On  a  manu- 
facturing scale,  coal  or  coke  is  substituted  for  the  charcoal. 
The  process  is  applicable  to  the  production  of  indium, 

VOL.  II.  B 


i8  MODERN   CHEMISTRY 

thallium,  germanium,  tin,  lead,  manganese,  iron,  cobalt, 
nickel,  and  copper.  To  exemplify  this  method,  four 
instances  will  be  described — the  preparation  of  phosphorus, 
sodium,  zinc,  and  iron. 

Phosphorus. — The  commonest  natural  compounds  of 
phosphorus  are  phosphorite  or  calcium  phosphate, 
Ca3(PO4)2,  and  gibbsite  or  aluminium  phosphate,  A1PO4. 
It  is  accordingly  convenient  and  economical  to  prepare 
phosphorus  from  one  of  them.  The  process  depends  on 
the  displacing  action  of  carbon  on  the  oxide  at  a  high 
temperature.  There  are  two  methods  of  effecting  this. 
The  first  is  :  the  phosphorite  is  mixed  with  dilute  sulphuric 
acid ;  the  hydrogen  of  the  sulphuric  acid  replaces  the  cal- 
cium of  the  calcium  phosphate:  Ca3(PO4)9  + 3H9SO4.Aq 
=  3CaSO4+ 2H3PO4.Aq.  Coke  or  charcoal  is  impreg- 
nated with  the  phosphoric  acid  and  heated  to  redness,  when 
the  phosphoric  acid  loses  water  :  HgPO4  =  HPOg  +  H2O. 
The  mixture  of  metaphosphoric  acid,  HPO3,  with  carbon 
is  charged  into  retorts  of  Stourbridge  clay,  the  mouths  of 
which  are  attached  to  a  vertical  copper  tube,  the  lower 
end  of  which  dips  under  water.  On  raising  the  retorts  to 
a  white  heat,  phosphorus  distils  over  and  condenses  in  the 
water.  The  final  equation  is  :  4HPO3+  I2C  =  2H2  +  P4 
+  I2CO.  By  the  second  method,  the  calcium  and  alumi- 
nium phosphates  are  mixed  with  silica  and  carbon,  and 
distilled  from  an  electric  furnace  heated  to  whiteness  by 
an  arc  in  its  interior. 

Sodium. — A  mixture  is  made  of  "spongy  iron"  (see 
p.  19)  and  pitch.  This  mixture  is  heated  to  redness  in 
order  to  decompose  the  pitch,  which  consists  of  compounds 
of  carbon  and  hydrogen.  These  compounds  are  decom- 
posed, and  a  part  of  the  carbon  is  left  mixed  with  the 
spongy  iron,  while  the  hydrogen  escapes  in  combination 
with  the  rest  of  the  carbon.  To  this  mixture,  placed  in 
an  iron  crucible,  caustic  soda  is  added  ;  the  lid  of  the 
crucible,  which  is  furnished  with  a  curved  tube  sloping 
downwards  to  a  condenser,  is  fixed  in  place,  and  the 


ZINC  AND    IRON  19 

crucible  is  heated  in  a  furnace  to  bright  redness.  The 
carbon  removes  oxygen  both  from  the  hydrogen  and  the 
sodium,  and  sodium  and  hydrogen  pass  over  into  the 
condenser  along  with  carbon  monoxide,  the  sodium  alone 
condensing,  for  the  others  are  gaseous  and  escape.  The 
equation  is:  2NaOH  +  zC  =  2CO  +  H2+  2Na.  The  con- 
denser consists  of  a  flat  hollow  copper  vessel ;  the  sodium 
is  raked  out  as  it  accumulates. 

Zinc. — The  chief  ore  of  zinc  is  the  sulphide.  To 
convert  it  into  the  oxide,  it  is  roasted  on  a  flat  hearth  in  a 
current  of  air  :  2ZnS  +  $O2=  2ZnO  +  2SO2.  The  oxide 
is  mixed  with  small  coal  (slack)  and  placed  in  cylindrical 
retorts  of  fireclay.  These  retorts  have  pipes  of  rolled 
sheet-iron  luted  to  the  open  ends  with  fireclay  ;  they  are 
packed  into  a  furnace  in  tiers,  and  the  temperature  is  raised 
to  bright  redness.  The  coal  distils  first,  giving  off  coal- 
gas,  which  expels  air  from  the  retorts.  When  the  tem- 
perature exceeds  1000°,  the  zinc  distils  and  condenses  in 
the  iron  pipes.  It  happens  that  almost  all  zinc  ores 
contain  cadmium  sulphide,  which,  like  zinc  sulphide,  is 
converted  into  oxide  by  roasting ;  and  on  distillation,  the 
cadmium,  which  is  the  more  volatile  metal,  distils  over 
first  and  condenses  in  the  outer  portion  of  the  tubes. 
These  are  untwisted  and  the  metal  removed  with  a  chisel. 

Iron. — The  chief  ores  of  iron  are  the  carbonate  and 
the  oxide.  The  former  is  practically  always  mixed  with 
clay  (clayband)  or  with  coal  (blackband),  and  generally 
contains  sulphur  and  phosphorus  in  the  form  of  calcium 
sulphate,  CaSO4,  and  calcium  phosphate,  Ca3(PO4)9. 
The  sulphur  is  sometimes  present  in  the  form  of  iron 
pyrites,  FeS2.  The  ore  is  roasted  to  expel  carbon 
dioxide,  thus:  4FeCO3  +  O2  =  2Fe2O3  +  4CO2.  If  it 
were  then  in  its  impure  state  smelted  with  coal,  the 
iron  would  not  flow,  but  would  remain  mixed  with  the 
clay.  However,  this  process,  if  the  ore  is  pure  and  charcoal 
is  used  as  fuel,  yields  a  mass  of  iron  sponge,  which  can  be 
heated  and  welded  by  hammering  into  a  coherent  mass. 


20  MODERN   CHEMISTRY 

The  process  is  still  used  by  Africans,  and  was  at  one  time 
universal.  On  the  large  scale,  however,  it  is  necessary  to 
add  lime  in  order  to  form  a  flux  with  the  clay.  Clay  con- 
sists of  a  compound  of  silica,  SiO0,  and  alumina,  A12O3, 
and  with  lime  it  melts  to  a  glassy  slag.  Alternate  layers 
of  coal,  lime,  and  the  roasted  ore  are  fed  in  at  the  top  of  a 
blast-furnace,  a  tall  conical  erection  of  firebrick,  strength- 
ened by  being  bound  with  iron  hoops ;  at  the  bottom  there 
is  a  "crucible,"  or  receptacle  for  the  molten  iron,  which 
can  be  discharged  when  required  by  forcing  a  hole  in  its 
side  with  an  iron  bar.  There  are  also  holes  which  admit 
water-jacketed  tubes  or  "tuyeres,"  which  convey  a  blast 
of  air  heated  to  about  600°  to  increase  the  temperature  of 
combustion  of  the  coal.  Here  the  reduction  takes  place 
in  the  upper  part  of  the  furnace,  owing  to  the  carbon 
monoxide  formed  by  the  combustion  of  the  coal  in  the 
lower  part  of  the  heated  mass ;  it  ac:s  on  the  oxide  of  iron 
thus:  Fe2O3+ 3CO  =  2Fe  + 3CO2.  As  the  iron  passes 
down  the  furnace  it  melts,  and  is  met  by  the  fused  slag  ; 
it  then  coheres  and  runs  into  the  crucible,  whence  it  is 
drawn  off  from  time  to  time. 

Carbon  unites  with  molten  iron,  forming  a  carbide ;  hence 
the  product  of  the  blast-furnace  is  not  pure  iron,  but  a 
mixture  of  iron  with  its  carbide,  and  also  with  its  sulphide 
and  phosphide,  if  the  ore  has  contained  sulphates  or  phos- 
phates. When  such  impure  iron  is  brought  in  contact 
with  oxygen  in  a  molten  or  semi-molten  condition,  the 
carbon,  sulphur,  and  phosphorus  are  oxidised  mostly  before 
the  iron.  If  lime  be  present,  sulphate  and  phosphate  of 
calcium  are  formed.  The  modern  process  of  removing 
these  impurities  is  to  pour  the  molten  metal  into  a  pear- 
shaped  iron  vessel  lined  with  bricks  made  of  magnesia  ; 
while  it  is  molten,  air  is  blown  through  the  metal,  and  the 
carbon  burns  to  carbon  dioxide ;  the  sulphur  and  phosphorus 
are  likewise  oxidised  and  combine  with  lime,  a  layer  of 
which  floats  on  the  surface  of  the  molten  metal.  When 
these  impurities  have  thus  been  removed  in  the  "  Bessemer 


DISPLACEMENT   BY  OXYGEN  21 

converter,"  the  metal  is  poured  into  a  mould.  Steel  is 
a  mixture  of  iron  with  a  trace  of  its  carbide,  and  it  is 
produced  by  mixing  with  the  blown  iron,  before  it  is 
poured,  a  quantity  of  iron  containing  carbon  and  manganese 
(a  metal  which  confers  valuable  properties  on  iron).  The 
quantity  of  carbon  in  steel  may  vary  between  O.6  and  1.5 
per  cent. ;  with  the  content  of  carbon  varies  also  the  quality 
of  the  steel ;  that  with  a  small  proportion  is  soft,  with 
a  high  proportion  hard. 

(e)  Displacement  by  means  of  Oxygen. — Oxygen 
is  used  in  Deacon's  process  to  liberate  chlorine  from 
hydrogen  chloride.  The  latter  gas,  mixed  with  air,  is 
passed  through  a  chamber  kept  between  the  limits  of 
temperature  375°-4OO°,  containing  bricks  soaked  with 
cupric  chloride,  CuCl0.  At  this  temperature  the  cupric 
chloride  decomposes  into  cuprous  chloride,  CuCl,  and 
free  chlorine,  but  the  cuprous  chloride  is  reconverted  into 
cupric  chloride  at  the  expense  of  the  chlorine  produced 
by  the  interaction  of  the  hydrogen  chloride  and  the  air, 
thus :  4HC1  +  O2  =  2H2O  +  2CI2.  The  cupric  chloride  is 
again  decomposed.  This  kind  of  action,  where  a  limited 
quantity  of  a  substance,  itself  not  permanently  changed, 
causes  an  apparently  unlimited  change  in  other  reacting 
bodies,  is  termed  "  surface  action,"  for  its  rate  is  dependent 
on  the  extent  of  the  surface  of  the  agent ;  and  the  name 
"catalysis"  is  sometimes  given  to  such  an  action.  The 
action  would  take  place  independently  of  the  catalytic 
agent,  but  at  a  very  slow  rate ;  the  presence  of  the  catalyser 
has  the  effect  of  greatly  increasing  the  rate  at  which  the 
change  takes  place.  The  chlorine  thus  prepared  is  not 
pure,  but  mixed  with  the  nitrogen  and  argon  of  the  air, 
but  it  serves  for  some  purposes.  The  rate  of  such  action 
of  oxygen  in  displacing  bromine  or  iodine  from  their 
compounds  with  hydrogen  is  much  greater,  and  at  a  high 
temperature  the  elements  could  be  formed  thus,  but  they 
are  not  usually  produced  in  this  way. 

The  preparation  of  nitrogen  may  be  also  regarded  as   a 


22  MODERN   CHEMISTRY 

displacement  by  means  of  oxygen.  Ammonia  burns  in 
oxygen,  thus:  3NH3+  $O2=  3H2O  +  N2,  but  at  the 
same  time  some  of  the  nitrogen  unites  with  the  oxygen 
and  forms  NO9,  nitric  peroxide :  this  gas  interacts  with  the 
ammonia,  forming  ammonium  nitrate  and  nitrite,  NH4NO3 
and  NH4NO9.  If,  however,  the  oxygen  be  not  free,  but 
in  combination  with  an  easily  reduced  metal,  such  as  copper, 
it  will  combine  with  the  hydrogen  of  the  ammonia  at  a  red 
heat,  setting  free  the  nitrogen.  Another  method  involves 
the  mutual  displacement  of  nitrogen  from  its  oxide  by 
means  of  hydrogen,  and  from  its  hydride,  ammonia,  by 
oxygen:  2NH3  +  N2O3=  3H2O  +  2N2.  This  method  is, 
however,  usually  represented  by  the  equation  NH4NO0  = 
2H2O  +  N2;  for  ammonium  nitrite,  NH4NO2,  may  be 
regarded  as  a  compound  of  N2O3  with  2NH3  and  H2O. 
To  obtain  nitrogen  by  this  method,  since  ammonium  nitrite 
is  not  easily  obtained,  a  solution  of  ammonium  chloride  may 
be  warmed  with  one  of  sodium  nitrite.  The  equation  is 
then  :  NaNO2.  Aq  +  NH4C1.  Aq  =  2H2O  +  N2  +  NaCl.  Aq. 
Another  convenient  method  is  to  warm  together  solu- 
tions of  sodium  hypobromite  and  ammonium  chloride  ;  the 
former  loses  oxygen  readily,  which  combines  with  the 
hydrogen  of  the  ammonia  according  to  the  equation : 
3NaOBr.Aq.  +  2NH4Cl.Aq.  =  sNaBr.Aq.  +  3H0O  + 

2HCl.Aq.  +  N2. 

Although  sulphur,  selenium,  and  tellurium  burn  in  oxy- 
gen, still  they  may  be  displaced  from  their  hydrides,  H2S, 
H2Se,  and  H0Te,  by  means  of  oxygen  at  a  red  heat, 
provided  the  oxygen  is  present  only  in  sufficient  quantity  to 
combine  with  the  hydrogen,  thus  :  2H2S -f  O2=2H2O  + 
S9.  Aqueous  solutions  of  these  compounds,  too,  are 
decomposed  on  standing,  in  contact  with  air,  owing  to 
similar  displacement.  Oxygen  may  displace  mercury  from 
its  sulphide,  cinnabar,  HgS,  which  is  the  common  ore  of 
mercury  ;  here  the  sulphide  is  roasted  in  air,  when  the 
sulphur  combines  with  the  oxygen  to  form  sulphur  dioxide, 
a  gas  at  ordinary  temperature ;  and  mercury  is  liberated. 


DISPLACEMENT   OF   ELEMENTS  25 

also  in  the  gaseous  form,  but  condensing  at  temperatures 
below  358°. 

(/)  Displacement  by  use  of  Fluorine,  Chlorine,  and 
Bromine. — Fluorine,  chlorine,  and  bromine  may  also  be 
employed  as  displacing  agents  for  nitrogen  and  oxygen. 

A  current  of  fluorine  led  through  water  displaces  the 
oxygen,  forming  hydrogen  fluoride ;  but  the  oxygen  is  in 
an  allotropic  state  (see  Part  i. ),  called  "ozone."  Again, 
if  a  stream  of  chlorine  is  passed  through,  or  if  bromine- 
water  be  added  to,  a  solution  of  ammonia,  the  hydrogen 
and  chlorine  combine,  while  the  nitrogen  is  set  free : 
2NH3.Aq  +  3C12  =  6HC1  +  N9;  but  as  ammonia  com- 
bines with  hydrogen  chloride,  the  reaction  6NH3  +  6HC1 
=  6NH4C1  occurs  simultaneously;  the  complete  equation 
is  the  sum  of  these  two  :  8NH3.  Aq  +  3d.,  =  6NH4C1. Aq 
+  N2. 

Chlorine,  added  to  a  solution  of  bromide  or  iodide  of  a 
metal,  displaces  the  bromine  or  iodine ;  here  the  non- 
ionised  chlorine  becomes  ionised  at  the  expense  of  the 
charge  on  the  ionised  bromine  or  iodine,  while  the  latter 

+  -  +  - 

lose  their  charges,  thus  :  2KBr.  Aq  +  C12.  Aq.  =  2KCl.Aq 
+  Br2. Aq.  Similarly,  bromine  displaces  iodine  from  a 
soluble  iodide.  But  iodine  displaces  chlorine  from  the 
nearly  insoluble  silver  chloride.  Here,  the  iodine  is  still 
less  soluble  than  the  chloride ;  and  as  chloride  dissolves, 
the  less  soluble  and  therefore  non-ionised  iodide  is  formed. 

(g)  Many  metals  are  able  to  displace  others.  Thus, 
iron  placed  in  a  solution  of  a  copper  salt  displaces  the 
copper ;  copper  displaces  silver ;  silver,  gold.  In  all 
these  cases  the  action  is  doubtless  an  electrical  one,  and 
dependent  on  the  replacement  of  a  metal  of  lower  by  one  of 
higher  electric  potential ;  that  of  higher  potential  becomes 
ionised,  while  that  of  lower  assumes  the  metallic  state, 

thus:  CuCl2.Aq  +  Fe  =  FeCl2.Aq  +  Cu;  2AgNO3.Aq  + 
Cu  -  Cu(NO3)2.  Aq  +  2  Ag. 


24  MODERN   CHEMISTRY 

(h}  There  are  some  plans  of  obtaining  elements  which, 
though  they  can  be  referred  to  one  or  other  of  the  three 
general  methods  exemplified  already,  are,  on  account  of 
their  complexity,  better  treated  separately.  Among  these 
are  the  methods  of  separating  hydrogen.  The  metals  of 
the  alkalies  and  alkaline  earths  attack  water,  forming  hydr- 
oxides and  liberating  hydrogen  :  zNa  +  2H9O  =  2NaOH  + 
H2;  Ca+  2H2O  =  Ca(OH)2  +  H9.  Magnesium  powder, 
boiled  with  water,  gives  off  hydrogen  slowly ;  but  zinc 
requires  the  presence  of  an  acid,  and  must  not  be  pure, 
i.e.  there  must  be  a  foreign  metal  present  to  serve  as  the 
anode.  The  impurity  usually  present  in  commercial  zinc 
is  lead ;  the  acid,  for  instance,  sulphuric  acid,  is  present  in 

r  +  + 

dilute  solution  as  ions  of  HH  and  SO4 ;  the  SO4  removes 

+  + 

the  surface  layer  of  the   zinc   as  Zn,   while   the   negative 
charge   is  transferred    to    the    lead,   which    is   in   metallic 
contact  with  the  zinc.     This  charge  is  neutralised  by  the 
»  +  + 

positive  charge  of  the  HH,  which,  on  being  discharged, 
escapes  in  an  non-ionised  state.  It  may  then  be  collected 
over  water,  in  which  it  is  very  sparingly  soluble.  Hydro- 
gen, while  it  is  on  the  point  of  discharging  and  is  still  in  the 
ionised  state,  may  be  used  to  liberate  certain  elements  from 
their  oxides  or  chlorides.  Zinc  and  hydrochloric  acid, 

I-  \+~ 

for  instance,  in  a  solution  of  stannous  chloride,  SnCl2.Aq, 

causes  a  deposition  of  tin  owing  to  the  exchange  of  charge  ; 
the  hydrogen  retaining  its  charge  instead  of  parting  with  it 
to  the  lead  or  other  impurity  in  the  zinc,  while  the  tin  is 
discharged  in  its  stead.  If  zinc  and  hydrochloric  acid  are 
placed  in  contact  with  silver  chloride,  AgCl,  which  is  an 
insoluble  compound,  the  hydrogen  remains  charged,  while 
the  silver  parts  with  the  chlorine,  the  latter  remaining  in 
solution  with  negative  charge.  Lastly,  if  generated  in  a 


solution  of  ferric  chloride,  Fe  Clg.Aq,  the  zinc  goes  into 
solution  as  before ;  and  the  positive  electricity  is  provided 


PROPERTIES  OF   ELEMENTS  25 

by  the  loss  of  a  positive  charge  provided  by  the  ferric  ions 

+  +  - 
changing  to  the  ferrous  ions  of  ferrous  chloride,  FeCl2.  Aq, 

+  - 

and  another  molecule  of  HCl.Aq  exists  in  solution.  The 
valency  of  the  iron  is  lowered.  Such  processes  are  gene- 
rally termed  reduction  ;  the  hydrogen  is  said  to  be  in  the 
"  nascent  state/'  and  is  named  the  "reducing  agent." 

Metallic  iron,  manganese,  cobalt,  and  nickel  at  a  red 
heat  remove  oxygen  from  water  with  liberation  of  hydro- 
gen:  3Fe  +  4H2O  =  Fe3O4  +  3H2;  2Co  +  2H2O  =  CoO 
+  O2.  Conversely,  a  current  of  hydrogen  passed  over 
these  oxides  at  a  red  heat  will  combine  with  their  oxygen, 
reducing  them  to  metal.  This  is  an  instance  of  mass- 
action.  From  the  equations  given  above,  it  is  seen  that 
hydrogen  is  formed ;  it  does  not  remain  in  the  tube  to 
re-form  water  ;  if  it  did,  there  would  be  a  state  of  balance 
or  equilibrium,  all  four  substances  remaining  together  in 
proportions  depending  on  the  temperature  and  on  their 
nature  ;  in  the  current  of  steam,  however,  the  hydrogen  is 
carried  on,  and  is  no  longer  present  to  act  on  the  oxide  of 
the  metal.  And  in  the  converse  action  the  hydrogen 
conveys  the  steam  away,  so  that  it  can  no  longer  be 
deprived  of  oxygen  by  the  metal. 

As  already  remarked,  carbon  monoxide  has  a  similar 
reducing  action  on  the  oxides  of  the  more  easily  reducible 
elements.  The  product  in  this  case  is  the  dioxide,  CO0, 
for  example,  Fe2O3+  3CO  =  2Fe  +  3CO2.  This  action 
requires  a  red  heat.  Another  reducing  agent,  applied  by- 
fusing  the  oxide  with  it,  is  potassium  cyanide,  KCN ; 
it  is  converted  into  the  cyanate,  KCNO.  The  metal 
thallium  may  be  prepared  by  its  help,  T19O  +  KCN  =  2T1 
+  KCNO.  As  the  cyanide  is  somewhat  expensive,  it  is 
used  only  in  special  cases. 

An  instance  has  already  been  given  of  the  mutual  reduc- 
tion of  two  compounds  in  the  case  of  nitrogen.  Similar 
instances  are  known  with  lead  and  with  sulphur.  The 
chief  ore  of  lead  is  the  sulphide,  a  natural  product  termed 


26  MODERN   CHEMISTRY 

galena.  It  is  roasted,  i.e.  heated  in  contact  with  air  to  a 
red  heat.  After  a  portion  has  been  oxidised  to  sulphate, 
PbS  +  2O9  =  PbSO4,  the  temperature  is  raised,  when  the 
sulphide  and  the  sulphate  mutually  reduce  each  other : 
PbS  +  PbSO4  =  2Pb  +  2SO2.  With  sulphur  the  partial 
burning  of  sulphuretted  hydrogen  may  be  explained  in  a 
similar  manner;  the  reaction,  2H2S  +  O9  =  2H2O  +  S0, 
may  be  represented  as  the  formation  of  water  and  sulphur 
dioxide  by  the  complete  combustion  of  one-half  of  the 
hydrogen  sulphide,  and  its  reaction  with  the  remaining 
sulphide,  thus:  2H2S  +  SO2=  2H2O  +  38.  And,  as  a 
matter  of  fact,  that  reaction  does  take  place  on  mixing 
the  two  gases  in  the  required  proportion  of  two  volumes 
of  hydrogen  sulphide  with  one  of  sulphur  dioxide. 

The  Properties  of  the  Elements. — It  has  been  cus- 
tomary to  divide  the  elements  into  two  classes,  the  metals 
and  the  non-metals.  As  we  have  seen,  this  classification 
is  a  completely  arbitrary  one ;  for  there  are  some  elements 
capable  of  existing  in  both  states.  The  name  "  metal " 
was  originally  given  to  seven  substances,  all  alike  in  possess- 
ing that  bright  lustre  known  as  "metallic."  These  were 
gold,  silver,  mercury,  copper,  iron,  lead,  and  tin.  But  in 
the  Middle  Ages  bismuth  and  antimony  were  isolated  in  a 
fairly  pure  state,  and  these,  together  with  zinc,  were  at  first 
not  received  into  the  class,  but  were  regarded  as  spurious ; 
for  they  were  brittle  and  easily  oxidisable.  Although 
there  is  no  reason  for  retaining  the  division,  yet  it  is  often 
convenient.  Bodies  which  possess  metallic  lustre  have  the 
power  of  conducting  electricity  better  than  transparent  bodies, 
and  they  are  also  relatively  good  conductors  of  heat. 

The  elements  exist  in  various  physical  states.  Those 
which  are  gases  at  the  ordinary  temperature,  however,  have 
all  been  condensed  to  the  liquid  state  by  sufficient  reduction 
of  temperature.  The  lowering  of  temperature  is  most  easily 
produced  by  means  of  liquid  air,  now  a  cheap  commodity. 
To  liquefy  air,  it  is  compressed  by  a  pump  to  a  pressure  of 
150  atmospheres ;  it  then  traverses  a  coil  of  copper  pipe, 


PROPERTIES   OF   ELEMENTS  27 

and  escapes  from  an  orifice  at  the  lower  end.  Now, 
compressed  air  has  some  resemblance  to  a  liquid,  for 
when  it  expands,  as  when  a  liquid  changes  to  gas,  heat  is 
absorbed.  The  rapidly  escaping  air  becomes  cold,  and  in 
passing  up  over  the  coil  of  tube  through  which  it  has  de- 
scended, it  cools  the  pipe,  so  that  the  air  passing  down 
becomes  colder  and  colder ;  finally,  it  is  so  cooled  that  it 
liquefies,  and  escapes  from  the  orifice  in  a  liquid  state.  It 
may  be  poured  from  one  vessel  to  another,  with  little  loss 
by  evaporation ;  and  if  other  gases  be  allowed  to  stream 
into  a  tube  cooled  by  its  aid,  they  too  are  liquefied.  The 
principle  of  liquefying  hydrogen  is  the  same,  for  its  boiling- 
point  lies  so  low  that  it  cannot  be  liquefied  by  the  aid  of 
liquid  air.  That  of  helium  is  still  lower,  but  it  too  has 
yielded  when  compressed  into  a  tube  cooled  by  liquid 
hydrogen. 

The  elements  which  are  gases  at  the  ordinary  temperature 
are  hydrogen,  helium,  neon,  argon,  krypton,  xenon,  nitro- 
gen, oxygen  and  ozone,  fluorine,  and  chlorine.  The  first 
seven  are  colourless,  both  in  the  gaseous  and  the  liquid 
state.  Oxygen  is  a  colourless  gas,  but  forms  a  pale  blue 
liquid ;  gaseous  ozone  has  a  blue  colour ;  fluorine  is  pale 
yellow ;  and  chlorine  has  a  greenish-yellow  colour.  It 
forms  a  white  solid,  which,  however,  melts  to  a  bright 
green  liquid.  Bromine  is  a  dark  red  liquid  at  atmospheric 
temperature,  but  above  its  boiling-point,  59°,  it  is  a  deep 
red  gas.  Iodine  is  a  blue-black  solid,  melting  to  a  black 
liquid  at  114°,  and  giving  off  a  violet  vapour.  Ozone  and 
the  "  halogens,"  as  fluorine,  chlorine,  bromine,  and  iodine 
are  called,  have  all  a  powerful  odour,  and  act  on  the  skin 
in  a  corrosive  manner.  Chlorine  and  bromine  are  soluble 
in  water. 

Among  the  other  non-metallic  elements  are  boron,  a 
black,  dusty,  infusible  powder ;  carbon,  in  its  ordinary  form 
an  amorphous  (i.e.  non-crystalline)  black  substance,  of  which 
the  most  familiar  variety  is  charcoal ;  carbon  does  not  fuse, 
but  at  the  enormously  high  temperature  of  the  electric  arc 


28  MODERN  CHEMISTRY 

it  volatilises  ;  silicon,  a  blackish-brown  powder,  melting  at 
bright  redness  to  a  lustrous  liquid,  which  solidifies  in  shining 
black  lumps  ;  phosphorus,  a  waxy,  pale  yellow  solid,  melt- 
ing at  44.4° ;  sulphur  and  selenium,  yellow  and  brown-red 
solids,  the  former  melting  at  115°  to  a  brown  liquid,  and 
boiling  at  446° ;  the  latter  forming  a  black  liquid  at  217°, 
and  a  black  vapour  at  665°. 

The  metals  of  the  alkalies,  as  they  are  usually  called, 
lithium,  sodium,  potassium,  rubidium,  and  cassium,  are  soft 
white  metals,  at  once  attacked  by  water,  and  oxidised 
readily  by  air,  caesium,  indeed,  taking  fire  spontaneously. 
To  protect  them  from  oxidation,  they  must  be  kept  under 
rock-oil  or  ligroin,  a  compound  which  contains  no  oxygen. 
Of  these,  caesium  has  the  lowest  and  lithium  the  highest 
melting-point.  The  metals  calcium,  strontium,  and  barium 
are  sometimes  named  the  "  metals  of  the  alkaline  earths." 
They  are  hard  white  bodies,  also,  like  those  of  the  sodium 
group,  oxidising  readily  on  exposure  to  air,  and  at  once 
attacked  by  water.  Magnesium,  zinc,  and  cadmium  are 
noteworthy,  inasmuch  as  their  temperature  of  ebullition  is 
not  so  high  that  it  cannot  be  reached  in  an  ordinary  furnace; 
they  can  therefore  be  distilled.  Magnesium  and  zinc  are 
hard  and  brittle ;  cadmium  is  softish,  like  lead,  and  of  a 
somewhat  greyer  tint. 

The  remaining  elements  may  be  classed  under  the  head- 
ings, "  hard,"  "  soft,"  "  brittle,"  &c.  This  implies  only 
their  behaviour  at  ordinary  temperatures ;  at  higher  or 
lower  temperatures  the  properties  are  materially  changed. 
Mercury,  for  example,  below  -40°,  is  malleable;  lead  is 
brittle. 

(a)  Malleable  metals  :— 

(1)  White^  ductile,  moderately  hard: — beryllium,  alumi- 
nium, gallium,   indium,   tin,  silver,  nickel.      Red,  copper. 
Tellow,  gold. 

(2)  Grey-white,    ductile,    and    moderately    hard: — iron, 
manganese,  cobalt. 


METALS  29 

(3)  G 'rey- white  and soft ;  ductile: — thallium,  lead ;  some- 
what  harder,  and  fusible  only  at  a  <very  high  temperature  : — 
rnodium,  ruthenium,  palladium,  platinum,  iridium. 

(  b  )   Liquid  metal : — mercury. 

(c]  Brittle  metals  : — 

(1)  White,  hard: — antimony,  bismuth,  tellurium,  zirco- 
nium, didymium   (a  mixture),  osmium,  germanium.      Less 
hard,  arsenic. 

(2)  Grey,  hard : — lanthanum,  cerium,  yttrium,  uranium. 

( 3 )  Grey  powders,  acquiring  metallic  lustre  under  the  bur- 
nisher : — thorium,  niobium,  tungsten. 

(4)  Black  powders  : — tantalum,  titanium. 

The  elements  scandium,  samarium,  and  gadolinium  have 
not  been  prepared. 

Although  the  external  properties  of  the  elements  does 
not  show  any  obvious  relation  to  their  order  in  the  periodic 
table  (see  Part  I.),  yet  it  may  be  generally  remarked  that 
the  density  increases  as  each  column  is  descended.  Among 
the  lightest  of  the  elements  are  lithium,  beryllium,  magnesium, 
and  aluminium,  at  least  in  the  solid  state  ;  whereas  osmium, 
iridium,  platinum,  and  gold  are  among  the  heaviest.  But 
much  more  must  be  ascertained  regarding  their  properties 
before  a  satisfactory  comparison  can  be  made. 


CHAPTER   II 
Classification  of  Compounds — The  Hydrides. 

Classification  of  Compounds. — Compounds  of  the 
elements  may  be  divided  conveniently  into  six  classes : — 

The  Hydrides  ; 

The  Halides  ; 

The  Oxides  and    Sulphides    (with  Selenides  and 

Tellurides)  ; 
The  Nitrides  and  Phosphides  (with  Arsenides  and 

Antimonides)  ; 

The  Borides,  Carbides,  and  Silicides ; 
The  Alloys. 

Compounds  can  be  prepared  by  many  methods  ;  it  is  not  so 
easy  to  classify  them  as  it  is  to  arrange  into  classes  the 
methods  of  preparation  of  elements.  As  a  rule,  the  pre- 
paration is  carried  out  by  one  of  the  following  methods  : — 

(a)  The  interaction  of  elements  ; 

(£)  The  action  of  an  element  on  a  compound  ; 

(c)  The  action  of  heat  on  a  compound  ; 

(d)  The  interaction  of  compounds  ; 

(e)  The  addition  of  one  compound  to  another. 

These  methods  shall  be  considered  in  relation  to  each  of  the 
groups  of  compounds  named  above. 

The  Hydrides. 

(a)  The  Interaction  of  Elements. — Lithium,  sodium, 
and  potassium,  when  heated  to  300°  in  an  iron  tube  in  a 


INTERACTION   OF   ELEMENTS  31 

current  of  hydrogen,  form  white  waxy  compounds  ;  that  of 
lithium  has  the  formula  LiH  ;  as  the  sodium  compound  has 
the  formula  Na9H,  its  existence  is  difficult  to  reconcile  with 
the  usual  valency  of  either  hydrogen  or  sodium,  for  these 
elements  in  all  other  compounds  behave  as  monads.  It  would 
repay  further  investigation.  It  decomposes  at  421°. 

Iron,  nickel,  palladium,  and  platinum,  when  heated 
gently  in  hydrogen,  absorb  the  gas.  Meteoric  iron,  indeed, 
has  been  known  to  give  off,  on  heating,  2.85  times  its 
volume  of  gas.  This  natural  variety  of  iron  contains  about 
6  per  cent,  of  nickel.  Palladium,  gently  warmed  in  an 
atmosphere  of  hydrogen,  absorbs  over  900  times  its  volume 
of  that  gas,  corresponding  to  4.68  per  cent,  of  the  weight 
of  the  body  produced.  It  is  difficult  to  determine  whether 
or  not  the  palladium  is  in  chemical  combination  with  the 
hydrogen,  or  whether  the  hydrogen  is  in  a  state  analogous 
to  solution,  for  it  is  known  that  a  solid  can  exert  solvent 
power.  There  is  a  considerable  rise  of  temperature  accom- 
panying the  absorption  ;  and  if  palladium,  in  a  state  of 
sponge,  is  placed  in  contact  with  a  mixture  of  oxygen  and 
hydrogen,  the  mixture  may  be  made  to  explode.  A  ther- 
mometer-bulb coated  with  palladium  sponge  is  a  good  test 
for  the  presence  of  an  explosive  mixture  of  marsh-gas  and 
air  in  mines,  for  the  rise  of  temperature  produced  is  an  in- 
dication of  danger.  These  metals  absorb  hydrogen  more 
readily  if  they  are  made  the  negative  electrodes  of  a 
battery  with  which  dilute  sulphuric  acid  is  electrolysed. 
Iron  shows  a  very  curious  behaviour  under  these  circum- 
stances. If  a  thin  plate  of  iron  is  made  to  close  the  top  of 
a  barometer-tube  full  of  mercury  and  a  small  cell  be  con- 
structed on  it,  hydrogen  will  pass  through  the  iron,  when 
the  plate  is  made  the  kathode,  and  will  depress  the  mer- 
cury in  the  tube.  No  other  metal,  so  far  as  is  known, 
shows  this  peculiarity  ;  it  would  appear  that  the  hydrogen 
in  the  ionic  state  can  penetrate  the  iron. 

Carbon,  heated  to  1200°  in  an  atmosphere  of  hydrogen, 
unites  with  it  to  form  marsh-gas  (methane),  CH4.  Only 


32  MODERN  CHEMISTRY 

a  small  percentage  of  the  hydrogen,  however,  enters  into 
combination  ;  a  balance  soon  establishes  itself  between  the 
number  of  molecules  of  methane  being  formed  and  decom- 
posed in  unit  time.  At  a  higher  temperature,  that  of  the 
electric  arc,  acetylene,  C2H2,  is  formed,  owing  to 
the  decomposition  of  the  methane  into  that  gas  and  free 
hydrogen: — 2CH4  =  C9H9  +  3Ht>.  Other  compounds  of 
carbon  and  hydrogen  are  formed  simultaneously,  and  there 
again  appears  to  be  a  state  of  equilibrium  produced  between 
the  various  hydrocarbons  formed.  With  nitrogen,  NH,, 
it  appears  to  be  impossible  to  induce  hydrogen  to  enter  into 
direct  combination  at  such  temperatures  ;  but  if  electric 
sparks  be  passed  through  a  mixture  of  hydrogen  and  nitro- 
gen, combination  to  a  limited  extent  ensues.  Should  the 
ammonia,  NH3,  be  removed  by  having  water,  or,  better, 
dilute  sulphuric  acid,  present,  the  combination  proceeds 
until  all  the  gases,  if  they  were  originally  present  in  the 
correct  proportion — one  volume  of  nitrogen  to  two  volumes 
of  hydrogen — have  combined.  Conversely,  if  sparks  be 
passed  through  ammonia  gas,  there  is  nearly,  but  not  quite, 
complete  decomposition  into  its  constituents.  This  enables 
the  volume  relations  of  ammonia  to  be  demonstrated  ;  for 
it  is  found  that  two  volumes  of  ammonia  gas  can  be  decom- 
posed into  two  volumes  of  nitrogen  and  six  volumes  of 
hydrogen.  This  is  symbolised  by  the  equation — 

2NH3  =  N2   +  sH, 

Weight  2 ( 14  + 3)      28         3  (2)  grams. 
Volume  2(22.4)         22.4      3(22.4)  litres. 

The  hydrogen  can  be  nearly  completely  removed  by  ab- 
sorption with  palladium-sponge,  and  the  nitrogen  remains. 

Water,  H20,  is  more  completely  formed  than  any  one 
of  the  previously  mentioned  compounds  by  the  interaction 
of  its  elements.  A  mixture  of  oxygen  and  hydrogen,  in 
the  proportion  of  one  volume  of  oxygen  to  two  of  hydrogen, 
is  exploded  by  heat ;  this  is  most  easily  done  by  passing  an 
electric  spark  through  the  mixture.  While  the  position  of 


COMBINATION  OF   HYDROGEN  33 

equilibrium  for  a  mixture  of  nitrogen,  hydrogen,  and  am- 
monia lies  at  such  a  point  that  very  little  of  the  compound 
is  present,  but  chiefly  the  uncombined  gases,  the  contrary  is 
the  case  with  hydrogen  and  oxygen.  Here  nearly  all  the 
oxygen  and  hydrogen  combine,  and  only  a  trace  remains 
uncombined.  Combination  may  be  made  to  take  place 
slowly  at  much  lower  temperatures  ;  even  at  300°  slow 
combination  occurs.  Colloidal  platinum,  prepared  by  mak- 
ing an  electric  arc  between  poles  of  platinum  under  pure 
water,  which  appears  to  consist  of  very  finely  divided 
platinum  disseminated  through  the  water,  has  the  power  of 
causing  union  of  oxygen  and  hydrogen  left  standing  in 
contact  with  it,  even  at  the  temperature  of  the  atmosphere. 
On  the  other  hand,  if  water-  vapour  be  raised  to  a  very  high 
temperature,  above  1800°,  decomposition  into  its  consti- 
tuents takes  place  with  considerable  rapidity  ;  so  that  it  is 
possible  to  obtain  a  mixture  of  oxygen  and  hydrogen  by 
passing  steam  through  a  tube  in  which  a  spiral  of  platinum 
wire  is  kept  at  a  white  heat  by  means  of  an  electric  current. 
These  actions  are  therefore  termed  "  reversible,"  and  they 
are  expressed  by  such  equations  as  — 

CH4  ^  C  +  2H9  ;          2H9  +  O.,  ^  2H20  ; 


Hydrogen  also  combines  with  sulphur  when  passed 
through  a  flask  containing  boiling  sulphur,  and  sulphuretted 
hydrogen,  H2S,  decomposes  when  raised  to  a  low  red 
heat. 

Interesting  relations  are  to  be  seen  with  the  compounds 
of  the  halogens  with  hydrogen.  In  preparing  fluorine  by 
the  electrolysis  of  hydrogen-potassium  fluoride,  KHF,  in 
presence  of  hydrogen  fluoride,  H2F9,  it  is  possible,  by  stop- 
ping the  exit  of  the  hydrogen,  to  cause  a  bubble  to  pass  the 
bend  of  the  U-tube  and  to  rise  into  the  fluorine  ;  the  instant 
the  gases  unite  there  is  a  sharp  explosion.  This  shows 
that  these  gases  unite  even  in  the  dark  to  form  H2F2. 
Chlorine  and  hydrogen,  on  the  other  hand,  do  not  com- 

VOL.  II.  C 


34  MODERN   CHEMISTRY 

bine  in  the  dark,  but,  when  exposed  to  diffused  daylight, 
slow  but  complete  combination  ensues  ;  in  bright  sunlight, 
or  when  illumined  by  the  light  from  burning  magnesium, 
the  mixture  of  gases  explodes,  forming  HC1.  Bromine  and 
hydrogen  unite  to  form  HBr  when  a  current  of  hydrogen, 
having  bubbled  through  a  wash-bottle  of  bromine,  passes 
through  a  red-hot  tube  ;  with  excess  of  hydrogen  the  union 
is  practically  complete.  Iodine  and  hydrogen,  on  the 
contrary,  unite  very  incompletely  to  produce  HI ;  and  if 
hydrogen  iodide  be  heated,  a  large  proportion  of  it  is 
decomposed  into  hydrogen  and  iodine.  This  change  has 
been  investigated  much  more  completely  than  other  changes 
of  the  same  character  already  mentioned ;  and  as  it  is 
characteristic  of  all  such  reversible  reactions,  we  shall  con- 
sider it  in  somewhat  greater  detail. 

The  rate  at  which  hydrogen  iodide  is  produced  from  a 
mixture  of  hydrogen  and  iodine  at  any  constant  tempera- 
ture is  much  more  rapid  than  that  at  which  the  reverse 
change  of  hydrogen  iodide  into  iodine  and  hydrogen  takes 
place.  This  rate  was  not  difficult  to  determine.  Weighed 
quantities  of  iodine  were  placed  in  a  tube  filled  with  hydro- 
gen, and  after  heating  the  sealed  tube  for  a  sufficiently  long 
time  for  equilibrium  to  be  established,  it  was  opened  under 
water.  The  hydrogen  iodide  formed  at  once  dissolved  in 
the  water,  and  the  residual  hydrogen  was  measured.  The 
amount  of  uncombined  iodine  remaining  in  the  water  was 
then  estimated  by  known  processes.  It  was  thus  possible 
to  find  the  ratio  of  the  combined  to  the  uncombined  hydro- 
gen. Now,  it  was  discovered  many  years  ago  that  the  rate 
of  chemical  change  depends  on  the  amount  of  each  of  the 
reacting  substances  present  in  unit  volume — a  condition  ex- 
pressed by  the  term  "active  mass."  Thus,  if  we  double 
the  amount  of  hydrogen  in  the  mixture  of  the  gases  men- 
tioned, we  double  its  "  active  mass/'  Let  /9  denote  the 
number  of  molecules  in  unit  volume  of  the  iodine  gas,  and 
^2  that  of  the  hydrogen,  and  let  ^hi  be  that  of  the  hydrogen 
iodide  formed  by  their  interaction.  Then,  as  the  rate  of 


HYDRIDES   OF   CARBON  35 

formation  of  hydrogen  iodide  is  proportional  both  to  /  and  to 
/>,  it  will  be  proportional  to  their  product,  h  x  /.  And  as 
H0  +  I9=  2 HI,  the  rate  of  change  of  HI  into  H2  and  I.? 
will  be  2hi  x  ihi  or  4(/>/)2.  If  we  call  the  rate  of  forma- 
tion k,  and  that  of  decomposition  /£',  the  proportion  of 
these  rates  to  each  other  will  be  kjk' =  (h  x  i)/4(»i)2,  if  the 
gases  are  present  in  molecular  proportions.  At  the  tem- 
perature 440°,  and  at  one  atmosphere  pressure,  it  was  found 
that,  taking  the  total  hydrogen  as  unity,  0.28  was  free 
and  0.72  combined,  after  a  sufficient  time  had  been  al- 
lowed for  the  change  to  complete  itself.  Now,  the  iodine 
free  must  have  been  equal  in  number  of  molecules  to  the 
free  hydrogen,  i.e.  0.28,  and  the  same  number  of  atoms 
of  iodine  must  have  existed  in  combination  as  of  hydro- 
gen in  combination;  hence  0.28x0.28/4(0.72x0.72) 
=  0.0375  =  ^/y£'.  This  means  that  at  440°  molecules  of 
hydrogen  iodide  decompose  into  hydrogen  and  iodine  at 
a  rate  only  0.0375  (or  one  twenty-sixth)  of  that  at  which 
combination  takes  place  between  the  two  gases. 

(b]  The  action  of  an  element  on  a  compound  leads 
to  the  formation  of  many  hydrides.     This  process  has  been 
pretty  fully  treated  in  the  description  of  the  methods  of 
preparation  of  elements.     For  example,  on  passing  a  current 
of  hydrogen  over  hot  cupric  oxide,  water,  H.,0,  is  formed, 
while    the    oxide    is    reduced    to    copper,    CuO  +  H9  = 
Cu  +  H2O.       The    oxides    mentioned   on    p.  16  are   thus 
reduced.     It  is  not  so  usual  for  sulphides  to  lose  sulphur  on 
heating  them  in  a  stream  of  hydrogen ;   indeed,  it  is  only 
those  sulphides  which  themselves  decompose  when  heated 
that  yield  to  such  treatment ;  but  hydrogen  fluoride,  chlo- 
ride, bromide,  and  iodide  are  formed  on  heating  the  halides 
of  many  metals  in  a  current  of  hydrogen.     The  process, 
however^  is  not  one  which  is  used  for  the  preparation  of 
these  hydrides. 

(c)  The  third  method — that  of  heating  a  compound — 
is  also  not  in  use  as  a  means  of  preparing  hydrides^  but  it 
is  often  employed  in  order  to  produce  the  compound  from 


36  MODERN   CHEMISTRY 

which  the  hydride  is  separated.  Thus,  all  compounds 
containing  water  of  crystallisation,  when  heated,  lose  water 
when  raised  to  a  high  temperature ;  and  double  compounds  of 
ammonia,  too,  lose  ammonia  on  rise  of  temperature.  Such 
compounds  as  calcium  chloride,  CaCl0,  crystallise  with 
water.  The  formula  of  the  hydrated  compound  is  CaClQ. 
6H2O  ;  a  similar  compound  with  ammonia,  CaCl0.6NH3, 
is  also  known  ;  compounds  like  these  lose  water  or  am- 
monia when  heated.  By  this  plan  Faraday  succeeded  in 
liquefying  ammonia,  which  at  ordinary  temperatures  is  a 
gas.  Having  sealed  up  the  ammonio-chloride  of  calcium  or 
of  silver,  AgCl.NH3,  in  an  inverted  U-tube,  one  leg  was 
cooled  with  a  freezing  mixture,  while  the  other  was  heated, 
and  the  gas  liquefied  under  the  combined  influence  of  cold 
and  pressure. 

(^/)  Most  of  the  hydrides  can  be  prepared  by  the  fourth 
method — the  interaction  of  compounds.  The  decom- 
posing agent  is  either  water,  an  acid,  or  an  alkali. 

(  i )  Water  : — Marsh-gas,  CH4,  ethylene,  C2H4,  acety- 
lene, C0H0,  ammonia,  NH3,  and  phosphoretted  hydrogen, 
PH3,  may  be  produced  by  the  action  of  water  on  some 
compounds  of  carbon,  nitrogen,  and  phosphorus.  Alumi- 
nium carbide,  A14C3,  yellow  transparent  crystals  produced 
by  heating  a  mixture  of  carbon  and  oxide  of  aluminium  to 
whiteness  in  the  electric  furnace,  on  treatment  with  water 
yields  pure  methane,  A14C3  +  1 2R,O  -  3CH4  +  4A1  ( OH)g. 
Manganese  carbide,  black  crystals  produced  by  heating  in 
the  electric  furnace  a  mixture  of  manganese  oxide  and 
carbon,  yields  a  mixture  of  equal  volumes  of  hydrogen 
and  methane,  Mn3C  +  6H2O  =  3Mn(OH)2  +  CH4  +  H2. 
Lithium,  calcium,  strontium,  and  barium  carbides  also 
formed  in  a  similar  manner  in  the  electric  furnace  yield 
acetylene  with  water,  Li9C.7  +  2H.7O  =  2LiOH  +  C9H9  ; 
CaC2  +  2H2O  =  Ca(OH)2+~C2H2;  The  carbides  of 
cerium,  CeC2,  lanthanum,  LaC9,  yttrium,  YC2,  and 
thorium,  ThC2,  yield  a  mixture  of  methane,  ethylene, 
C.7H4,  and  acetylene,  sometimes  mixed  with  hydrogen  ; 


INTERACTION   OF  COMPOUNDS  37 

and  uranium  carbide,  U2C2,  gives  methane,  ethylene,   and 
hydrogen,  but  no  acetylene. 

Magnesium  or  calcium  nitrides,  prepared  by  heating 
metallic  magnesium  or  calcium  in  a  current  of  nitrogen, 
yield  ammonia  with  water:  Mg3N2  +  6H2O  =  2NH3  -f 
3Mg(OH).>,  and  calcium  phosphide,  produced  by  heat- 
ing lime  with  phosphorus,  on  treatment  with  water  simi- 
larly gives  off  phosphoretted  hydrogen  :  CagP2  +  6H2O  = 
3Ca(OH)0  +  2PH3.  The  sulphides  of  magnesium  and 
aluminium,  MgS  and  A19S3,  are  also  decomposed  by  water, 
with  production  of  hydrogen  sulphide  and  the  hydroxide 
of  the  metal :  MgS  +  2H.OH  =  Mg(OH)9  +  H2S  ;  A1.,S3 
+  6H.OH  =  2Al(OH)g  +  3H2S. 

The  halides  of  a  certain  number  of  elements  are  at  once 
decomposed  by  water  with  formation  of  a  hydride  of  the 
halogen  and  a  hydroxide  of  the  element.  Boron,  silicon, 
titanium,  phosphorus,  sulphur,  selenium,  and  tellurium 
chlorides,  bromides,  and  iodides  are  thus  resolved.  The 
method  is  practically  made  use  of  in  preparing  hydrogen 
bromide,  HBr,  and  iodide,  HI,  by  help  of  phosphorus. 
But  the  previous  preparation  of  phosphorus  bromide  or 
iodide  is  unnecessary.  It  is  sufficient  to  add  bromine  to 
water  in  contact  with  red  phosphorus,  and  hydrogen  bro- 
mide is  evolved  ;  or  to  warm  a  mixture  of  iodine,  water, 
and  red  phosphorus.  The  use  of  yellow  phosphorus  is  not 
advisable,  for  the  action  is  apt  to  take  place  too  violently  if 
it  be  used.  It  may  be  supposed  that  the  phosphorus  and 
halogen  unite  to  form  the  pentahalide,  which  is  then  imme- 
diately decomposed  by  the  water,  thus  :  PBr.(or  PI6)  + 
4H,O  =  H3PO4+5HBr(or  sHI).  The  gaseous  hydride 
may  be  collected  over  mercury  or  by  downward  displace- 
ment, or  it  may  be  dissolved  in  water  and  a  solution  of 
hydrobromic  or  hydriodic  acid  prepared. 

A  commercial  method  of  producing  hydrogen  chloride, 
HC1,  depending  on  the  decomposition  of  magnesium 
chloride  when  heated  in  a  current  of  steam,  has  been 
patented ;  it  results  in  the  formation  of  a  compound  of 


38  MODERN  CHEMISTRY 

oxide  and  chloride  of  magnesium,  while  the  hydrogen  of 
the  water  unites  with  a  part  of  the  chlorine  ;  the  resulting 
gaseous  hydrogen  chloride  is  passed  up  towers,  and  comes 
into  contact  with  water,  thus  yielding  a  solution  of  hydro- 
chloric acid. 

(2)  In  many  cases  the  compound  from  which  the  hydride 
is  formed  is  not  decomposed  by  water  ;  an  acid,  generally 
hydrochloric  acid,  must  be  present.  The  reason  of  this  is 

+ 
not  easily  explained  ;  it  may  be  that  the  very  few  ions  of  H 

and  OH  present  in  water  are  sufficient  to  effect  the  decom- 
position in  some  cases  and  not  in  others,  and  that  when 
an  acid  is  necessary  the  much  larger  number  of  ions  of 
hydrogen  present  in  its  solution  is  required  ;  also  it  is 
known  that  the  heat  evolved  during  the  decomposition 
of  those  compounds  which  are  altered  by  water  is 
greater  than  that  which  would  be  evolved  by  those  which 
resist  its  action  were  they  to  be  attacked  by  water. 
Many  hydrides  are  prepared  by  the  help  of  acids.  Mag- 
nesium boride,  Mg3B.,,  yields  with  hydrochloric  acid  a  trace 
of  BH3  ;  but  as  this  compound  is  a  very  unstable  gas, 
almost  all  of  it  decomposes  into  boron  and  hydrogen.  The 
similar  compound,  Mg9Si,  produced  by  heating  a  mixture 
of  silica  and  magnesium  powder  to  redness,  when  mixed 
with  hydrochloric  acid  yields  hydride  of  silicon,  SiH4,  as 
a  colourless,  spontaneously  inflammable  gas  :  —  Mg2Si  + 
4HC1.  Aq  =  2MgCl2  Aq  +  SiH4.  Arseniuretted  hydrogen, 
AsH3,  and  antimoniuretted  hydrogen,  SbH3,  are  prepared 
from  sodium  or  zinc  arsenide  or  antimonide  :  Na3  As  + 
3HCl.Aq  =  3NaCl.Aq  +  AsH3  ;  Zn3Sb2  +  6HCl.Aq  = 
3ZnCl9.Aq  +  2SbH3.  These  gases,  however,  may  be  ob- 
tained mixed  with  hydrogen  if  a  solution  of  oxide  of  arsenic 
or  antimony  in  hydrochloric  acid,  which  yields  chloride  of 
arsenic  or  antimony,  is  treated  with  zinc.  The  first  change 
is  the  replacement  of  the  zinc  by  the  arsenic  or  antimony, 

" 


thus  :  2  AsCl3.  Aq  +  3Zn  =  3ZnCl2  Aq  +  2  As.     Electrically 


HYDRIDES  39 

neutral  zinc  replaces  positively  charged  arsenic,  itself  be- 
coming positively  charged.  The  arsenic  and  the  unattacked 
zinc  form  a  couple,  and  the  hydrochloric  acid  is  electrolysed, 

+  -  +  +     ++  -  + 

2HC1.  Aq  +  Zn  =  ZnCl2.  Aq  +  2H  ;  the  hydrogen  ion  unites 
with  the  arsenic,  negatively  charged  in  the  electric  couple, 
forming  electrically  neutral  hydride  of  arsenic,  which  escapes 

+ 

as  gas,  3  H  +  As  =  AsH3.  An  element  in  this  form,  capable 
of  combination  at  the  moment  of  liberation,  is  said  to  be  in  the 
nascent  state,  a  word  derived  from  "  nascere,"  to  be  born. 
It  differs  from  an  ordinary  element  in  being  on  the  point  of 
losing  an  electric  charge,  and  it  may  either  be  evolved  in 

+       + 

the  free  state  by  combining  with  itself,  as  H  +  H  =  H2,  on 
giving  up  its  charge,  or  it  may  enter  into  some  other  form 
of  combination,  as  in  the  case  explained.  This  process  of 
preparing  arsenic  or  antimony  hydride  is  used  as  a  test  for 
the  elements  arsensic  or  antimony.  It  was  devised  by 
Marsh,  and  as  the  hydrides  are  very  easily  decomposed 
by  a  high  temperature,  the  gas,  if  caused  to  pass  through  a 
red-hot  tube,  is  decomposed,  giving  a  deposit  of  arsenic 
(grey)  or  antimony  (black).  The  former  is  more  easily 
oxidised  than  the  latter,  and  dissolves  in  a  solution  of 
bleaching-powder,  in  which  the  latter  is  insoluble.  This 
process  is  particularly  applicable  where  poisoning  with 
arsenic  or  antimony  is  suspected. 

H.2S,  H2Se,  H2Te.  —  Hydrogen  sulphide,  selenide,  and 
telluride  are  prepared  by  treating  a  sulphide,  selenide,  or 
telluride  with  dilute  sulphuric  or  hydrochloric  acid  :  FeS 

+  H9SO4.Aq  -  FeSO4.Aq  +  H2S  ;  Sb0S3  +  6HCl.Aq 


=  2SbCl3.Aq  +  3H2S.     Na2Se.Aq  +  H2SO4.Aq  = 

Na2SO4.Aq  +  H2Se. 

Adds.  —  Hyd'ride  of  fluorine,  chlorine,  bromine,  and 
iodine,  when  dissolved  in  water,  are  termed  "acids."  As 
already  mentioned,  this  name  was  originally  applied  to  com- 


40  MODERN   CHEMISTRY 

pounds  which  possess  a  sharp  taste  and  change  the  colour 
of  certain  vegetable  colouring  matters.  The  word  was 
later  extended  to  apply  to  compounds  similar  in  function, 
although  not  acid  to  taste,  which  attack  the  carbonates, 
causing  them  to  effervesce,  and  which  yield  salts  with  the 
oxides  of  metals.  All  acids  contain  hydrogen,  and  it  is 
now  possible  to  define  them  in  a  very  simple  manner.  An 
acid,  in  fact,  is  a  compound  which  yields  hydrogen  ions 
when  dissolved  in  water,  or  in  some  other  solvent  capable 
of  causing  ionisation.  This  definition  applies  to  the 
hydrides  of  fluorine,  chlorine,  bromine,  and  iodine ;  and 
also  to  those  of  sulphur,  selenium,  and  tellurium  ;  for  on 

•f-  +  -  +- 

solution  they  ionise  thus  :   HF.Aq  ;   HCl.Aq  ;   HBr.  Aq  ; 

HLAq;  H.SH.Aq;  H.SeH. Aq ;  H.TeH.Aq.  But 
it  is  not  confined  to  them,  for  the  hydrogen  may  be  united, 
not  with  a  simple  element,  but  with  a  complex  group  of 

+  + 

elements,  as  in  H9SO4.Aq  or  HNO3.Aq.  Now,  in  dilute 
solution,  a  solution  of  sulphuric  acid  is  less  ionised  than  one 
of  hydrochloric  acid,  in  about  the  proportion  of  1:2,  and 
it  is  therefore  a  weaker  acid  ;  so  that  if  a  hydroxide,  such 
as  sodium  hydroxide,  be  presented  to  a  mixture  of  equal 
numbers  of  these  molecules,  in  quantity  requisite  for  only 
one  of  them,  chloride  of  sodium  will  be  formed  in  greater 
quantity  than  sodium  sulphate  ;  yet,  on  heating  a 
halide  with  sulphuric  acid,  because  hydrogen  chloride 
is  a  volatile  compound,  it  removes  itself  from  the  sphere 
of  action  in  a  non-ionised  state  while  the  sodium 
remains  as  sulphate.  Hence  these  hydrides  may  be  thus 
prepared.  Hydrogen  fluoride,  H2F2,  is  generally  prepared  by 
distilling  calcium  fluoride,  a  compound  naturally  occurring 
as  "  fluor-spar,"  with  sulphuric  acid  in  vessels  of  lead  or 
platinum:  CaF2  + H2SO4- BaSO4  + H2F2.  The  use  of 
lead  or  platinum  is  obligatory  on  account  of  the  action 
of  hydrogen  fluoride  on  glass  or  porcelain,  the  materials 
of  which  flasks  and  retorts  are  usually  made  ;  for 


HALIDES  41 

hydrogen  fluoride  attacks  the  silica  which  they  contain, 
forming  with  it  silicon  fluoride:  SiO2  +  2H2F2  =  SiF^  + 
2H9O.  Gold  is  almost  the  only  other  metal  which  resists 
the  action  of  hydrogen  fluoride.  There  is  no  such  diffi- 
culty with  the  other  halides.  Hydrogen  chloride,  HC1,  is 
prepared  by  distilling  from  a  glass  retort  a  mixture  of 
common  salt  and  oil  of  vitriol :  NaCl  +  H.7SO4  =  HNaSO4 
+  HC1.  On  a  large  scale  this  preparation  is  carried  out 
in  rotating  circular  furnaces,  the  mixture  of  salt  and  vitriol 
being  delivered  in  through  a  hopper  above,  and  at  the  high 
temperature  the  action  goes  further,  and  di-sodium  sulphate 
is  produced:  2 NaCl  +  H2SO4  =  NaaSO4+  2HCL  The 
gas  is  passed  up  towers  filled  with  coke,  and  exposed  to  a 
descending  stream  of  water,  in  which  it  dissolves,  forming 
a  saturated  solution  of  hydrochloric  acid,  or,  as  it  used  to 
be  called,  "muriatic  acid"  (from  "muria,"  brine). 

Hydrogen  bromide,  HBr,  and  iodide,  HI,  may  similarly  be 
produced  by  distilling  together  bromide  or  iodide  of  sodium  or 
potassium  with  exactly  the  right  weight  of  sulphuric  acid  for 
the  equation  2KBr  (or  zKI)  +  H2SO4.Aq=  K2SO4.Aq  + 
2HBr  (or  2HI).  But  in  these  cases,  the  hydrogen  bromide 
or  iodide  is  very  apt  to  exert  a  reducing  action  on  the  sul- 
phuric acid,  depriving  it  of  an  atom  of  oxygen,  thus :  — 
H2SO4  +  2HI  -  H2SO3  +  H2O  +  I2.  Hence  it  is  advis- 
abfe  to  use  phosphoric  acid,  H3PO4,  a  compound  not  thus 
reduced  :— H3PO4  +  2KI  =  H'K2PO4  +  2 HI. 

All  these  halides  come  over  as  gases,  and  may  either  be 
collected  over  mercury  or  by  "  downward  displacement," 
i.e.  by  delivering  them  to  the  bottom  of  a  jar  containing 
air,  which  owing  to  its  less  density  is  forced  upwards,  and 
escapes  at  the  mouth  of  the  jar.  They  cannot  be  collected 
over  water,  for  they  are  readily  soluble  in  it. 

The  compound  HN3,  termed  hydrazoic  acid  (from  the 
French  term  for  nitrogen,  "azote"),  is  also  liberated  in 
the  gaseous  form  by  warming  its  sodium  salt  with  sulphuric 
acid.  It,  too,  is  readily  soluble  in  water. 

(3)   Certain  hydrides  are  set  free  by  the  action  of  an 


42  MODERN   CHEMISTRY 

alkali,  i.e.  the  hydroxide  of  one  of  the  metals  of  the  sodium 
or  the  calcium  group.  It  is  true  that  the  change  may  be 
produced  by  other  hydroxides,  but  they  are  not  so  efficient, 
and  not  so  generally  employed.  Among  these  are  ammonia, 
NHg,  and  hydrazine,  NJH4.  These  bodies  unite  with 
acids  ;  for  example,  ammonia  and  hydrogen  chloride  form 
ammonium  chloride,  NH4C1,  when  mixed: — NH3  +  HC1 
=  NH4C1.  This  compound  is  produced  by  a  change  in 
valency  of  the  nitrogen  atom  ;  in  ammonia  it  is  a  triad,  N'", 
but  on  union  with  hydrogen  chloride  the  valency  of  the 
nitrogen  becomes  five,  Nv.  On  distillation  of  a  mixture  of 
ammonium  chloride  with  caustic  soda  or  with  slaked  lime, 
either  in  presence  or  absence  of  water,  the  following  change 
occurs  :— NH4C1  +  Na  O  H  =  NaCl  +  NH3  +  H2O  ; 
2NH4Cl  +  Ca(OH)2  =  CaCl2  +  2NH3+2H2O.  The 
initial  change  is  the  formation  of  ammonium  hydroxide, 
NH4OH  ;  this  substance,  being  unstable  when  heated, 
decomposes  into  ammonia  and  water.  Hydrazine,  a  com- 
pound of  the  formula  N0H4,  is  similarly  liberated  from  its 
chloride. 

The  usual  source  of  commercial  ammonia  is  coal-gas. 
On  distillation  of  coal,  all  varieties  of  which  contain  nitrogen, 
it  may  be  imagined  that  when  methane,  the  principal  consti- 
tuent of  coal-gas,  is  strongly  heated  it  splits  into  carbon  and 
hydrogen.  This  hydrogen,  at  the  moment  of  its  formation, 
is  in  the  nascent  state,  and  it  unites  with  the  nitrogen,  which 
is  also  in  the  nascent  condition.  As  ammonia  is  very  easily 
soluble  in  water,  while  the  other  constituents  of  coal-gas  are 
sparingly  soluble,  the  gas  is  deprived  of  ammonia  by  passing 
it  through  "  scrubbers,"  pipes  containing  broken  bricks  kept 
moist  with  water.  The  ammonia  dissolves,  while  the  coal- 
gas  passes  on.  The  solution  is  next  mixed  with  hydro- 
chloric acid  and  evaporated  to  dryness.  The  residue  of 
ammonium  chloride  is  then  distilled  with  lime,  as  previously 
described.  The  ammonia  is  received  in  water,  and  brought 
into  the  market  in  the  form  of  a  concentrated  solution,  to 
which  the  name  "  liquor  ammoniac  "  is  given. 


PROPERTIES  OF   HYDRIDES  43 

(b)  Certain  double  hydrides  are  formed  by  the  addition 
of  one  hydride  to  another.  Ammonia  and  hydrazine  unite 
with  hydrides  of  the  halogens  to  form  salts,  such  as  ammo- 
nium chloride,  NH4C1  ;  but  as  these  bodies  show  analogy 
with  salts  of  the  metals,  they  will  be  reserved  until  the  latter 
are  considered. 

General  Nature  of  the  Hydrides. — Hydrides  of 
lithium,  sodium,  potassium,  iron,  nickel,  palladium, 
and  platinum  differ  from  the  others  in  character  ;  they  are 
solid  bodies,  decomposed  by  heat.  Graham,  indeed,  who 
investigated  that  of  palladium,  was  struck  with  the  metallic 
nature  of  the  substance,  and  was  inclined  to  believe  that  it 
might  be  regarded  as  an  alloy  of  a  metallic  form  of  hydrogen, 
to  which  he  gave  the  name  "  hydrogenium ; "  and  it  was  for 
long  believed  that  liquid  hydrogen  would  show  the  character- 
istic property  of  metals,  metallic  lustre.  But  this  anticipation 
has  not  been  fulfilled.  Liquid  hydrogen  is  a  colourless  body ; 
and  solid  hydrogen  is  described  as  having  a  white  crystalline 
appearance,  like  ice  froth.  But  it  must  be  confessed  that 
hydrogen  shows  a  marked  similarity  to  metals  in  many  of  its 
compounds,  as  will  be  frequently  seen  in  the  sequel. 

The  remaining  hydrides  may  be  divided  into  three 
classes  : — Those  which  react  with  neither  acid  nor  bases, 
and  which  may  therefore  be  described  as  neutral.  To  this 
class  belong  the  hydrides  of  boron,  carbon,  silicon, 
arsenic,  and  antimony.  That  of  phosphorus  nearly  falls 
into  the  same  category,  for  its  compounds  with  acids  are 
very  unstable.  The  next  class — those  which  react  with 
bases — comprises  water  and  the  hydrides  of  sulphur, 
selenium,  and  tellurium.  The  compounds  are  termed 
hydroxides,  or,  in  the  case  of  sulphur,  hydrosulphides. 
These  will  be  considered  later,  but  an  instance  may  be  given 
here  : — When  lime  is  moistened  with  water  it  is  slaked, 
with  formation  of  calcium  hydroxide,  thus  :  CaO  +  H2O  = 
Ca  ( OH )  2.  The  hydrides  of  fluorine,  chlorine,  bromine, 
and  iodine  also  belong  to  this  class  ;  but  in  their  case  an 
exchange  takes  place,  thus  :  CuO  +  2HCl.Aq  =  CuCl2.Aq 


44  MODERN   CHEMISTRY 

=  H9O.  Hydrazoic  acid  is  capable  of  similar  reactions. 
Such  hydrides,  with  the  exception  of  water,  are  generally 
termed  acids.  The  last  group  of  hydrides,  ammonia  and 
hydrazine,  and,  in  one  or  two  isolated  cases,  hydrogen  phos- 
phide, unite  with  acids,  forming  salts,  thus  :  NH3  +  HC1  = 
NH4C1;  PH3  +  HI  =  PH4I.  It  appears  that  the  pre- 
sence of  water  is  necessary  for  at  least  the  first  of  these 
combinations  ;  for  if  perfectly  dry  hydrogen  chloride  is 
mixed  with  perfectly  dry  ammonia,  no  combination  results. 
It  is  perhaps  allowable  to  suppose  that  the  presence  of 
moisture  leads  to  ionisation  of  the  hydrogen  chloride,  and 
that  the  ionised  molecule  is  capable  of  entering  into  com- 
bination, while  the  non-ionised  molecule  is  without  action 
on  the  ammonia.  These  compounds  will  be  treated  of 
under  the  heading  of  "  salts." 

The  hydrides  of  boron,  carbon,  silicon,  phosphorus, 
arsenic,  and  antimony  are  insoluble  in  water ;  those  of 
nitrogen,  sulphur,  selenium,  tellurium,  and  the  halo- 
gens are  soluble.  With  the  exception  of  certain  hydrides 
of  carbon,  to  be  afterwards  described,  and  water,  all  the 
rest  are  gases  at  atmospheric  temperature.  The  fact  that 
water  is  a  liquid,  and  not,  as  might  be  expected,  a  gas,  re- 
quires comment.  It  is  noteworthy  that  water-gas  possesses 
the  density  9,  corresponding  to  the  molecular  weight  1 8  ; 
hence  there  can  be  no  doubt  that  in  the  gaseous  state  water 
has  the  formula  H9O.  But  it  is  known  that  compounds  of 
sulphur,  which  are  in  formulae,  and  in  many  properties 
analogous  to  compounds  of  oxygen,  possess  higher  boiling- 
points  than  the  corresponding  oxygen  compounds.  For 
instance,  bisulphide  of  carbon,  CS2,  boils  at  44°,  whereas 
carbon  dioxide  boils  at  about  —80°.  But  water  boils  at 
100°,  and,  contrary  to  expectation,  its  analogue,  sulphuretted 
hydrogen,  condenses  to  a  liquid  at  a  temperature  much 
below  o°.  Now,  it  has  been  found  by  a  method  depend- 
ing on  the  rise  of  liquids  in  capillary  tubes,  that  while  the 
molecular  weight  of  most  substances  in  the  state  of  liquid  is 
identical  with  those  which  they  possess  in  the  gaseous  state, 


HYDROCARBONS  45 

the  molecular  weight  of  water  is  considerably  too  great. 
The  conclusion  follows,  therefore,  that  the  molecular 
weight  of  water  should  be  expressed  by  a  more  complex 
formula  than  H2O  ;  possibly  by  H4O2,  or  by  one  even 
more  complex.  Gaseous  hydrogen  fluoride,  unlike  its 
congeners,  has  a  higher  molecular  weight  than  that  ex- 
pressed by  the  formula  HF  ;  determination  of  its  density 
leads  to  the  formula  H2F2.  These  facts  are  probably  to  be 
explained  by  the  view  that  oxygen  may  possess  a  higher 
valency  than  2,  and  fluorine  than  I,  at  relatively  low  tem- 
peratures. It  is  not  unlikely  that  the  structural  formula  of 

H\       /H 

liquid    water    is          >O=O<       ,  and  that  of  hydrogen 

H/  \H 

fluoride  HF=FH,  where  oxygen  acts  as  a  tetrad  and 
fluorine  as  a  triad. 

Hydrocarbons.  —  The  hydrides  of  carbon,  or 
"  hydrocarbons,"  are  very  numerous,  and  form  an  im- 
portant group  of  substances.  In  many  respects  they  are 
analogous  to  the  metals,  and  they  yield  derivatives  com- 
parable with  those  of  the  metals.  The  preparation  of  some 
of  them  has  already  been  described  ;  but  in  order  to  give  a 
more  complete  idea  of  their  structure  and  functions,  a  short 
description  of  other  methods  of  forming  them  is  annexed. 

Methane  or  marsh-gas,  if  mixed  with  its  own  volume  of 
chlorine,  and  exposed  to  daylight — not  sunlight,  else  the 
mixture  would  explode — undergoes  the  reaction  CH4  + 
C12  =  CH3C1  +  HC1.  The  resulting  gas,  termed  chloro- 
methane,  is  soluble  in  ether,  a  volatile  liquid  compound 
of  carbon,  hydrogen,  and  oxygen.  If  pieces  of  metallic 
sodium  are  added  to  the  solution,  the  sodium  withdraws 
chlorine  from  the  chloromethane  and  a  gas  is  evolved. 
On  analysis,  it  gives  numbers  answering  to  the  formula 
CH3.  But  if  that  were  its  formula,  its  molecular  weight 
in  grammes  would  occupy  22.4  litres;  but  15  grammes 
occupy  only  11.2  litres;  hence  its  molecular  weight  must 
be  30,  and  not  15,  and  its  formula  cannot-be  CH3,  but  must 


46  MODERN   CHEMISTRY 

be  C2H6.     It  is  reasonable  to  suppose  that  the  mechanism  of 

H\  : ;  /H 

the  reaction  is  this  :    H— ,C— :C1  +  Na  Na  +  Cl— C—  H  ; 

__  H/  \H 

and  that  the  two  CH3  groups  on  liberation  join  together, 

H\  /H 

forming  the   complex  group,  H— ~C — C — H.      Similarly, 

H/          \H 

mixing  C9H6,  which  is  named  ethane,  with  its  own 
volume  of  chlorine,  a  reaction  takes  place  like  that  with 
methane,  and  chlorethane  is  formed,  thus :  C2H6  +  C12  = 
C9H5C1  +  HC1.  Chlorethane  dissolved  in  ether  and  treated 
with  sodium  yields  not  C2H5  but  C4H10,  and  it  may  be 
supposed  that  the  constitution  of  the  new  hydrocarbon, 

H    H    H    H 
butane,  is  HC — C — C — CH.      A  mixture  of  chloro- 

H    H    H    H 
methane  and  chlorethane  gives  with  sodium  an  intermediate 

H    H    H 
hydrocarbon,    CJHL,    propane,    HC — C — CH.      When 

H    H    H 

chlorine  and  propane  are  mixed  in  equal  volumes,  two 
chloropropanes  result;  they  have  identical  formulas  and 
molecular  weights,  and  it  is  believed  that  the  difference 
between  them  consists  in  the  position  of  the  entering  atom 
of  chlorine.  In  one  case  the  chlorine  replaces  hydrogen 
attached  to  one  of  the  terminal  atoms  of  carbon,  thus  : 

H    H    H 

Cl  C — C — CH,  while  in  the  other  the  medial  hydrogen  is 
H    H    H 

H    Cl   H 
replaced  :     HC — C — CH.       These    two    chloropropanes 

H    H    H 

yield  in  their  turn  two  methylpropanes  or  butanes. 
Two  such  substances  are  said  to  be  isomeric,  or  to  exhibit 
isomerism  with  each  other.  The  following  list  gives  the 
names  and  formulae  of  some  of  this  series  of  hydrocarbons  ; 


HYDROCARBONS 


47 


where  the  difference  between  their  formulae  is  CH2,  they 
are  said  to  form  a  "  homologous  series." 


H 
HCH 

H 
Methane. 

H     H    H 

HC— C— CH 

H     H    H 

Propane. 

H     H    H 

HC— C— CH 

H      |      H 

HCH 

H 
Isobutane. 

H 
HCH 

|      H    H 
HC— C— CH 

|      H    H 
HCH 

H 
Isopentane. 


H    H 

HC— CH 

H    H 

Ethane. 

H     H    H    H 

HC— C— C— CH 

H     H    H    H 

Butane. 

H     H    H    H    H 

HC— C— C— C— CH 

H     H    H    H    H 

Pentane. 

H 

HCH 

H      |      H 

HC— C— CH 

H      |      H 

HCH 

H 
Tetramethyl-methane. 


Chloromethane,  if  mixed  with  its  own  volume  of  chlorine 
and  exposed  to  light,  yields  a  dichloromethane,  thus  : 
CH3C1  +  C12  =  CH?C12  +  HC1.  This  compound,  which, 
like  chloromethane,  is  also  a  gas  soluble  in  ether,  on  treating 
its  solution  with  sodium,  loses  chlorine  and  is  converted 
into  ethylene,  thus:  CH9C19  +  4Na  +  C19CH9  =  4NaCl 

H    H 
+  C=C .      The  carbon  atom,  it  will  be  observed,  is  still 

H    H 
a  tetrad,  but  the  two  atoms  are  connected  by  a  "  double 


48  MODERN   CHEMISTRY 

bond."     Homologues  of  ethylene  are  known,  of  which  the 
following  are  a  few  :  — 

H     H  H    H    H 

C=C  HC— C=C 

H     H  H           H 

Ethylene.  Propylene. 

HHHH          HHHH  H  H 

HC— C— C=C       HC— C=C— CH       HC— C— CH 

HHHH  H  H      ||     H 

HCH 

Butylenes. 

These  hydrocarbons  are  characterised  by  the  facility  with 
which  they  combine  with  the  halogens,  forming  oils  ;  they 
have,  therefore,  been  termed  "defines,"  or  "  oil-makers.'* 
They  also  unite  with  nascent  hydrogen,  and  are  converted 
into  paraffins,  as  the  members  of  the  former  group  are 
termed.  The  equations  which  follow  illustrate  this  : — 

H2C     Cl     H9CC1         CH.,  CH3 

1+1=1  ||     "  +  2tt=  | 

H2C     Cl     H,CC1         CH2  CH3 

By  the  further  action  of  chlorine  on  dichloromethane, 
trichloromethane,  or  chloroform,  CHC13,  is  produced. 
Chlorine  can  also  be  withdrawn  from  chloroform  by  sodium, 
and  acetylene,  C2H2,  is  formed:  HCCl3  +  6Na  +  Cl3CH 
=  6NaCl  +  HC=CH.  Here  the  two  carbon  atoms  are 
represented  as  united  by  a  treble  bond,  and  each  carbon 
atom  is  still  believed  to  remain  tetrad.  Acetylene  is 
also  characterised  by  the  ease  with  which  it  unites  with 
chlorine,  forming  a  tetrachlorethane  :  HC^CH  +  2C12  = 
C19HC— CHC13.  Here,  also,  other  members  of  the  series 
are  known. 

The  passage  of  acetylene  through  ^  red-hot  tube  is 
attended  by  "  polymerisation  ;  "  that  is,  two  or  more  mole- 
cules unite  to  form  a  more  complex  one.  In  this  case,  three 


HYDROCARBONS  49 

molecules  of  acetylene  combine  to  form  a  molecule  of  the 
formula  C6H6,  a  compound  to  which  the  name  benzene  is 
applied.  It  is  produced  in  large  quantity  by  the  distillation 
of  coal,  and  is  separated  from  coal-tar  oil  by  distillation. 
Its  carbon  atoms  are  imagined  to  form  a  ring,  because, 
among  other  reasons,  it  yields  only  one  mono-chloro-sub- 

H    H    H 

C— C=C 
stitution    product :       ||  gives    on    treatment    with 

C— C=C 

H    H    H 
H    H    Cl 
C— C=C 
chlorine,  C19,    ||  |    ;    and  as  all  the  hydrogen  atoms 

^  c_ c=c 

H    H    H 

in  the  molecule  are  symmetrically  arranged  with  respect  to 
the  carbon  atoms,  this  condition  is  fulfilled. 

The  four  first  members  of  the  methane  series  are  gases  ; 
those  containing  a  greater  number  of  atoms  of  carbon  up 
to  eleven  are  liquids,  and  the  higher  members  are  solids. 
The  paraffin  oil  which  is  burned  in  lamps  consists  of  a 
mixture  of  the  liquid  members,  and  paraffin  candles  largely 
consist  of  the  solid  members.  They  are  all  practically 
insoluble  in  water.  The  olefines  have  similar  physical  pro- 
perties, and  benzene  is  a  volatile  liquid.  Iodine,  sulphur, 
and  phosphorus  dissolve  in  the  liquid  hydrocarbons. 

These  and  other  hydrocarbons  may  be  considered  as 
somewhat  analogous  to  the  metals  ;  the  analogy  appears  in 
the  methods  of  formation  and  formulas  of  their  derivatives. 


CHAPTER   III 

The  Halides  of  the  Elements— Double  Halides 
— Endothermic  Combinations — Hydrolysis 
— Oxidation  and  Reduction — Mass=Action. 

The  Halides. — Compounds  of  fluorine,  chlorine,  bro- 
mine, and  iodine  are  thus  named.  They  fall  into  classes 
when  the  elements  are  arranged  according  to  the  periodic 
system.  Taking  the  chlorides  as  typical  of  the  halides, 
we  have  the  following  table  :  — 


LiCl 
NaCl 

BeCl2 
MgCl2 

BC13 
A1C13 

CC14 
SiCl4 

NC13 
PC15     PC13     SF6 

sci4' 

OC12 
SC12 

HC1 
...     FC1? 
...     C1C1 

KC1 
RbCl 
CsCl 

CaCl2 
SrCl2 
BaCl2 

ScCl3 
YC13 
LaCl3 

TiCl4 
ZrCl4 
CeCl4 

ThCl4 

...       AsCl3       ... 
SbCl5   SbCl3 
ErCl3       ... 
BiCl3 

SeCl4 
TeCl4 

TeCl2 

IC13      IC1 

CuCl 
AgCl 

ZnCl, 
CdCl2 

GdCl, 
HgCf2 

GaCl3 
InCl3 

Tici3 

GeCl4 

SnCl4 
TbCl4 
PbCl4 

VC15    VC1, 
NbCl5NbCl3      ... 
...       PrCU        ... 
TaCl3      ...     WC16 

MoCl4 

WC14 

CrCl2 
MoCl2 
NdCl2 
WC12 

MnCl3  ... 

FeCl3     Fed., 
RuCl3    RuCl2 

CoCls    CoCl2 
...      RuCl3        ... 

PdCl4 

NiCl2 
PdCU 

OsCl4      OsCl3     OsCl.2    IrCl4     IrCl3          ...       PtCl4        ...       PtCl2 

50 


THE   HALIDES  51 

Besides  these  compounds,  which  present  considerable 
regularity,  others  exist  which  have  less  claim  to  order. 
Thus,  KI3  is  also  known  ;  it  is  unstable,  but  CsI3  is  re- 
latively stable.  Again,  CuCl2  and  AuClg  exist,  also 
HgCJ.  In  the  next  group,  GaCl9,  InCl,  and  InCl2  are  also 
known,  as  well  as  T1C1.  The  following  group  contains 
SnCl.,  and  PbCl2  ;  PbCl4  is  very  unstable.  Besides 
VCl/and  VC13,  VC14  and  VC12  are  also  known  ;  and  in 
the  next  group,  CrCl3,  MoCl3,  and  MoCl5,  also  WC15, 
UC13,  and  UC15.  These  compounds  are  difficult  to 
classify. 

The  bromides  and  iodides,  as  well  as  the  fluorides,  corre- 
sponding to  many  of  these  chlorides  in  formula,  are  also 
known.  Where  they  are  of  special  interest,  they  will  be 
alluded  to  in  the  sequel. 

The  characteristic  of  the  halides  of  the  elements  of 
the  lithium  group  is  that  they  are  all  soluble  white  salts, 
crystallising  in  cubes.  In  dilute  solution  they  are  all  ion- 
ised, and  even  in  strong  solution  a  large  percentage  of  ions 
are  present.  Hence  they  all  react  as  metal  ions  and  as  halo- 
gen ions.  Thus,  for  instance,  with  silver  nitrate,  which  is 
the  usual  test  for  ionic  chlorine,  the  following  reaction  takes 

place  :  —  NaCl.  Aq  +  AgNO3.  Aq  =  NaNOg. Aq  +  AgCL 
Practically  insoluble,  and  therefore  practically  non-ionised, 
silver  chloride  is  precipitated,  and  free  ions  of  sodium  and 
the  nitrate  group  remain  in  solution.  If  concentrated 
solutions  are  mixed,  that  portion  which  is  ionised  reacts ; 
and  as  it  is  removed  from  solution,  the  originally  non- 
ionised  molecules  of  sodium  chloride  are  ionised,  because 
the  solution  becomes  more  dilute  as  regards  sodium  chloride, 
and  they,  too,  enter  into  reaction.  In  a  similar  way,  the 
alkali  metal  ions  react  in  presence  of  a  suitable  reagent. 
Another  point  to  be  noticed  is  that  these  salts  are  not 
hydrolysed,  that  is,  do  not  react  with  water  to  give  hydroxide 
and  acid  to  any  appreciable  extent,  and  the  usual  method 
of  preparing  them  depends  on  these  facts.  They  may 


52  MODERN   CHEMISTRY 

all   be  obtained   by  the   addition  of  halogen  acids  to  the 
hydroxides  or  carbonates  of  the  metals  dissolved  in  water, 


thus:  KOH.Aq  +  HBr.Aq-KBr.Aq  +  H2O.  It  will 
be  noticed  that  the  water  is  not  ionised,  nor  does  it  hydro- 
lyse  the  potassium  bromide  ;  hence,  on  evaporation,  as 
concentration  increases,  the  number  of  ions  of  potassium 
and  bromine  becomes  fewer  and  fewer,  and  after  the 
water  has  been  removed  the  pure  dry  salt  is  left.  With 
a'  carbonate  the  action  is  similar.  The  equation  is  : 

U2CO3.Aq  +  2HI.Aq  =  2LiL  Aq  +  H2O  +  CO2.  In 
dilute  solution  the  acid  H2CO3  would  be  liberated  ;  it  is  a 
very  weak  acid,  /'.<?.  it  is  comparatively  very  slightly  ionised  into 

+ 

2H.Aq  and  CO3.Aq  ;  and,  moreover,  it  readily  decom- 
poses into  H2O  and  CO2  ;  hence  it  is  removed  from  the 
sphere  of  action  as  it  is  formed,  and  on  evaporation  the 
salt  is  left  behind,  as  in  the  previous  example. 

Sodium  and  potassium  chlorides  occur  in  nature  ;  the 
former  in  the  sea,  which  contains  from  3.8  to  3.9  per  cent. 
Deposits,  which  have  undoubtedly  been  formed  by  the  drying 
up  of  inland  seas,  are  found  in  many  places.  At  Stassfurth  in 
S.  Germany  there  are  large  deposits  of  all  the  salts  present  in 
sea-  water,  including  common  salt,  chlorides  and  sulphates  of 
magnesium,  potassium,  and  sodium,  and  calcium  sulphate  ; 
these  have  been  deposited  in  layers  in  the  order  of  their 
solubilities,  the  less  soluble  salts  being  deposited  first. 
Bromides  and  iodides  are  also  present  in  minute  quantity  in 
the  residues  from  the  evaporation  of  sea-  water. 

Solutions  of  the  halides  of  the  beryllium  group  of  elements 
can  also  be  made  by  acting  on  the  hydroxides  or  carbonates 
of  the  metals  with  the  halogen  acid.  To  take  barium  chlo- 

+  +-  +  -  ++- 

ride  as  an  example,  BaCO3.Aq+  2HCl.Aq  =  BaCl2.Aq 
+  H2O  +  CO2.  Now  barium  carbonate  is  nearly  insol- 
uble in  water,  but  the  portion  which  dissolves  is  ionised  ; 
and,  as  explained  above,  when  the  portion  which  is  ionised  has 


THE   HALIDES  53 

reacted,  its  place  is  taken  by  more  of  the  carbonate  entering 
into  solution  ;  so  that  finally  all  is  changed  into  chloride. 
With  the  hydroxides,  the  same  kind  of  reaction  takes  place  : 

Ca(OH)9.Aq  +  zHBr.Aq  ==  CaBr^Aq  +  2H,O. 
These  salts  are  also  white  and  soluble  in  water.  There  is, 
however,  one  exception,  namely,  calcium  fluoride,  CaF9, 
which  occurs  native  as  fluor-  or  Derbyshire  spar.  It  forms 
colourless  cubical  crystals,  and  is  the  chief  compound  of 

+  +  - 
fluorine.      It   is    produced    by    precipitation:  CaCl9.Aq  + 


q  =  CaF2H-2KCLAq.  The  calcium  fluoride  is 
non-ionised,  and  comes  down  in  an  insoluble  form. 

Water  of  Crystallisation.  —  The  other  halides  of 
this  group  crystallise  with  water  of  crystallisation  ;  its 
amount  varies  from  7  molecules,  as  in  BaI9.yH9O,  to  I  as  in 
ZnCl9.H9O.  The  retention  of  this  so-called  "  water  of 
crystallisation  "  has  not  yet  been  satisfactorily  explained. 
It  was  for  long  believed  that  such  compounds  were  "  mole- 
cular/' as  opposed  to  atomic  ;  that  is,  that  the  water 
molecules  combined  as  wholes  with  the  salt,  and  not  by 
virtue  of  their  atoms  ;  but  it  is  more  probably  to  be  explained 
by  the  tetravalency  of  oxygen,  although  even  with  this 
assumption  it  is  not  easy  to  ascribe  satisfactory  constitutional 
formulas  in  all  cases.  It  must  at  the  same  time  be  assumed 
that  the  halogen  atoms  are  of  a  higher  valency  than  unity  ; 
possibly  triad,  or  even  pentad. 

These  salts  are  hydrolysed  in  solution  to  a  small  extent  ; 
thus  a  solution  of  magnesium  chloride,  besides  containing  a 
large  number  of  ions,  has  also  reacted  with  the  water  to  form 
hydroxide  and  hydrogen  chloride:  MgCl9  +  2H(OH) 
=  Mg(OH)2  +  2HC1.  As  the  solution  becomes  con- 
centrated on  evaporation,  the  hydrogen  chloride  volati- 
lises with  a  part  of  the  water  ;  and  a  mixture,  or  rather  a 
compound,  of  the  oxide  and  chloride  remains.  Hence  these 
chlorides  cannot  be  obtained  in  a  pure  state  by  evaporating 
their  solutions.  They  exhibit  another  property,  however, 


54  MODERN   CHEMISTRY 

which  makes  it  possible  to  obtain  them  in  a  pure  state, 
namely,  the  power  of  forming  "  double  halides."  This  pro- 
perty is  not  well  marked  with  the  halides  of  calcium,  barium, 
and  strontium,  but  the  halides  of  beryllium,  magnesium, 
zinc,  and  cadmium  are  notable  in  this  respect.  We  have, 
for  example,  MgCl2.KC1.6H2O,  ZnCl2.NH4Cl,  and  many 
similar  bodies.  In  solution,  such  compounds  are  mainly 
ionised  into  their  simple  ions,  but  on  evaporation  the  non- 
ionised  salt  separates  in  crystals,  and  is  not  subject  to 
hydrolysis.  Hence  such  salts  can  be  dried  without  decom- 
position. The  ammonium  salts,  when  sufficiently  heated, 
lose  ammonia  and  hydrogen  chloride  by  volatilisation,  and 
the  anhydrous  halide  is  left]:  MgCl2.NH4Cl  =  MgCl2  + 
NH3  -f  HC1.  The  mode  of  combination  of  these  double 
salts  is  possibly  owing  to  the  fact  that  the  halogens  are 


capable  of  acting  as  triads  ;    thus  Zn/  may  be 


taken  as  the  constitutional  formula  of  that  particular  salt. 

The  mono-halides  of  copper,  silver,  and  gold  may  be 
attached  to  the  first  group  ;  and  if  that  is  done,  the  mono- 
halides  of  mercury  must  also  be  included.  These  com- 
pounds are  all  insoluble  in  water,  and  are  consequently 
obtained  by  precipitation  or  by  heating  the  higher  halides, 
where  these  exist.  Thus  CuCl  and  AuCl  are  obtained 
by  cautiously  heating  CuCl2  and  AuCl3  ;  they  are  white 
insoluble  powders.  Cuprous  chloride  is  more  easily 
obtained  by  removing  half  the  chlorine  from  cupric  chloride 
dissolved  in  concentrated  hydrochloric  acid,  by  digesting 
it  with  metallic  copper:  CuCl2.2HCl.Aq  +  zHCl.Aq 
+  Cu  =  Cu2Cl2.4HCl.Aq,  a  brown  compound,  which  is 
decomposed  by  water  into  Cu9Cl9  and  4HCl.Aq  ;  the 
cuprous  chloride  is  thrown  down  as  a  snow-white  powder. 
With  silver  and  mercury,  the  chlorides  AgCl  and  HgCl  are 
formed  by  precipitation  from  the  respective  nitrates,  AgNO3 
and  HgNO3,  on  addition  of  soluble  chlorides.  The  bromides 
and  iodides  are  similarly  formed,  and  are  also  insoluble. 


THE   HALIDES  55 

There  are  several  interesting  points  connected  with  these 
halides.  First,  as  regards  their  colour;  the  chlorides  are 
white;  cuprous  bromide  is  greenish  brown,  while  the  brom- 
ides of  silver,  gold,  and  mercury  are  yellow ;  and  cuprous 
iodide  is  brownish,  and  the  iodides  of  the  other  metals  darker 
yellow  than  the  bromides.  It  appears  as  if  the  colour  was 
influenced  both  by  the- metal  and  by  the  halogen.  Next, 
the  chlorides  of  copper  and  mercury  give  evidence  of 
possessing  the  double  formulae  Cu2Cl2  and  Hg2Cl2,  which 
would  imply  that  the  metals  were  only  pseudo-monads, 
and  that  the  structural  formulas  should  be  Cl— Cu— Cu— Cl 
and  Cl— Hg— Hg— Cl  ;  and  this  would  correspond  with 
the  fact  that  the  chlorides  CuCl2  and  HgCl2  are  also 
known  ;  but,  on  the  other  hand,  as  AgCl  in  the  state  of  gas 
has  the  simple  formula  given  to  it,  it  may  be  that  it  is  the 
halogen  which  forms  the  bond  of  union  between  the  two 
half- molecules,  thus  :  CuCl=ClCu.  Silver  forms  no  higher 
halides. 

The  fluorides  of  these  elements  differ  from  the  others  in 
being  soluble  in  water  ;  they  are  prepared  from  the  oxides 
with  hydrofluoric  acid.  They  are  very  difficult  to  dry, 
for  they  undergo  the  reverse  reaction,  and  are  hydrolysed 
into  oxide  and  hydrogen  fluoride  on  evaporation. 

Copper  and  mercury  also  function  as  dyads ;  that  is, 
their  ions  are  capable  of  carrying  a  double  electric  charge 
under  certain  circumstances.  What  the  mechanism  of  this 
change  is,  we  do  not  know  ;  but  the  change  in  valency  can 
be  induced  by  presenting  to  the  element  a  larger  amount  of 
halogen,  if  it  is  desired  to  increase  the  valency,  or  by  remov- 
ing halogen  if  the  opposite  change  is  required.  The  addition 
of  halogen  to  the  mono-halide  is  in  each  case  an  exothermic 
change,  and  its  converse  is  an  endothermic  one.  Cuprous 
or  mercurous  chloride,  heated  in  a  current  of  chlorine 
changes  to  cupric  or  mercuric  chloride,  and  the  converse 
change  can  be  brought  about  by  heating  the  higher  halide 
in  a  current  of  hydrogen,  or  by  exposing  the  lower  halide 
to  the  action  of  nascent  hydrogen ;  but  it  is  difficult  to 


56  MODERN   CHEMISTRY 

prevent  the  action  in  the  latter  case  from  going  too  far  and 
yielding  the  metal.  A  solution  of  cupric  chloride  saturated 
with  sulphurous  acid  in  presence  of  hydrochloric  acid,  and 
then  diluted  with  water,  gives  a  precipitate  of  cuprous 
chloride :  2CuCl2. Aq  +  H2SO3. Aq  +  2HC1. Aq  +  H2O  = 
Cu2Cl2.4HCl.Aq  +  H9SO4.Aq.  The  sulphurous  acid  re- 
moves oxygen  from  water,  liberating  hydrogen  in  presence 
of  the  cupric  chloride,  and  the  latter  is  deprived  of  half 
its  chlorine  and  reduced  to  cuprous  chloride.  Similarly, 
stannous  chloride  forms  a  reducing  agent  for  mercuric 
chloride  :  2HgCl2.  Aq  +  SnCl2.  Aq  =  Hg2Cl2  +  SnCl4.  Aq. 
The  converse  change  can  be  produced  by  exposing  the  lower 
halide  in  presence  of  halogen  acid  to  the  action  of  nascent 
oxygen  :  Cu2Cl2  +  zHCl.Aq  +  O  -  iCuCL,. Aq  +  H2O. 
This  oxygen  in  the  case  of  copper  may  be  molecular,  O9, 
but  for  the  formation  of  the  higher  halide  of  mercury,  it 
must  be  derived  from  some  substance  capable  of  parting 
readily  with  oxygen,  such  as  nitric  acid. 

Cupric  iodide  is  very  unstable,  and  readily  yields  up 
iodine,  forming  cuprous  iodide.  On  mixing  cupric  chloride 
with  potassium  iodide,  the  cuprous  iodide  is  precipitated  : 

2CuCl2.  Aq  +  4-KI.  Aq  -  Cu2I2  +  4KCl.Aq  +  I2.  It  is  to 
be  noticed  that  the  dyad  cupric  ions  have  lost  two  charges, 
ancl  that  these  have  neutralised  the  two  negative  charges  of 
the  iodine  ions,  causing  them  to  be  precipitated.  (Inasmuch 
as  the  cuprous  iodide  is  insoluble,  it  should  not  have  had  the 
ionic  signs  attached ;  but  they  have  been  kept  in  order  to 
show  the  changed  valency. )  Mercuric  iodide  is  an  insoluble 
scarlet  precipitate,  and  is  therefore  best  produced  by  pre- 
cipitation. It  dissolves,  however,  in  a  solution  of  potassium 
iodide,  forming  a  double  salt,  of  which  more  shortly. 

Auric  chloride  contains  triad  gold,  and  thus  has  the 
formula  AuCl3.  It  is  not  produced  by  the  direct  action 
of  chlorine  on  gold,  because  the  temperature  of  attack  is 
above  the  temperature  at  which  the  compound  is  decomposed. 
But  it  is  possible  to  volatilise  gold  in  a  current  of  chlorine, 


THE   HALIDES  57 

because  a  few  molecules  escape  decomposition  and  are 
volatilised  along  the  tube  through  which  the  chlorine  is 
passed,  and  on  cooling  the  gold  is  deposited,  owing  to  the 
decomposition  of  the  chloride  at  a  lower  temperature.  It 
may  appear  paradoxical  that  the  chloride  is  stable  at  a 
higher  temperature  than  that  at  which  it  decomposes  ;  but 
it  is  to  be  presumed  that  the  difference  of  temperature 
between  one  favourable  to  an  exothermic  and  to  an  endo- 
thermic  action  is  very  small  ;  and  as  endothermic  substances 
increase  in  stability  on  rise  of  temperature,  the  chloride  is 
capable  of  volatilisation  ;  on  cooling  it  becomes  unstable  and 
undergoes  decomposition  with  deposition  of  gold.  The 
usual  method  of  preparing  this  salt  is  to  dissolve  gold  in 
a  mixture  of  nitric  and  hydrochloric  acids.  This  mixture 
yields  ionic  chlorine,  the  negative  charge  of  which  neutralises 
the  positive  charges  of  the  gold  ;  but  there  are  corresponding 
negative  charges  set  free,  which  are  transferred  to  the  ion 

NO3  of  the  nitric  acid,  converting  it  into  2O,  with  its  four 
negative  charges.  The  latter  combines  with  the  hydrogen, 

+  -        +    - 
forming  electrically  neutral  water:    3HC1  +  HNO3.Aq  + 


Au  =  2H2O  +  Au  C13  .  Aq  +  NO. 

Auric  chloride  forms  dark  red  crystals  ;  it  is  soluble  in 
water,  and  when  mixed  with  chlorides  of  the  alkali  metals 
forms  a  set  of  salts  termed  aurichlorides.  The  potassium 
salt,  for  example,  has  the  formula  K  AuCl4  ;  it  is  soluble  in 
water,  but,  unlike  the  "double  salts/'  such  as  MgCl2,2KCJ, 
already  alluded  to,  it  is  ionised  by  water,  not  into  simple 

+ 
ions  like  these,  but  into  the  ions  K  and  the  complex  group 

AuCl4.  At  the  same  time  there  exists  in  the  solution  a  small 
number  of  simple  ions,  so  that  on  electrolysis  gold  is  deposited 
at  the  kathode,  but  the  primary  effect  of  the  current  is  to 
send  the  aurichloric  ions  to  the  anode.  The  solution  of  mer- 
curic iodide  in  potassium  iodide,  of  which  mention  was 
madebefore,is  a  half-way  example  of  the  same  kind.  Its  solu- 


58  MODERN   CHEMISTRY 

+ 
tibn  contains  ions  of  K  and  HgI3,  but  these  are  mixed  with 

+ 

a  much  larger  proportion  of  the  simple  ions,  K  and  I  and 
i-  + 

Hg  and  I2.     Ail  grades  of  such  salts  are  known  ;  indeed  it 
is  probable  that  the  double  salts,  such  as  magnesium-potassium 

chloride,  contain  a  small  number  of  complex  ions  of  MgClg. 

These  halides  have  been  considered  at  length  because 
they  form  types  of  the  others.  Use  will  be  made  of  the 
examples  given  in  treating  of  the  remaining  halides. 

We  have  seen  that  the  halides  may  undergo  either  ionisa- 
tion  or  hydrolysis,  or  both  at  once.  The  ionisation  may  be 
more  or  less  complete,  and  the  hydrolysis  is  promoted  by 
dilution  and  by  a  high  temperature.  The  remaining  halides 
display  both  these  kinds  of  behaviour,  and  according  as  one 
or  the  other  prevails,  the  methods  of  preparing  them  are 
affected.  In  certain  cases,  moreover,  the  halides  form 
compounds  with  other  halides,  usually  those  of  the  alkali 
metals  or  hydrogen,  which  are  less  apt  to  be  hydrolysed, 
and  yield  different  complex  ions.  The  halides  of  carbon  and 
nitrogen  belong  to  neither  of  these  classes,  for  they  are 
insoluble  in  and  unacted  on  by  water.  As  neither  carbon 
nor  nitrogen  is  acted  on  by  the  halogens  (excepting  that 
carbon  burns  in  fluorine),  they  must  be  prepared  indirectly 
by  acting  on  one  of  their  compounds  with  the  halogen. 
Methane  or  carbon  disulphide  is  chosen  for  the  former,  and 
ammonia  in  preparing  the  latter.  By  passing  a  current  of 
chlorine  saturated  with  the  vapour  of  carbon  disulphide 
through  a  red-hot  tube,  the  chlorides  of  both  carbon  and 
sulphur  are  formed:  CS2  +  3C12  =  CC14  +  S2C12.  On 
treatment  with  water  the  sulphur  chloride  is  decomposed, 
while  the  chloride  of  carbon  may  be  distilled  off ;  it  forms 
a  colourless  liquid  boiling  at  76.7°.  Its  smell  resembles 
that  of  the  closely  allied  chloroform,  CHCJ3,  and  it  is  also 
possessed  of  anaesthetic  properties.  For  the  preparation  of 
nitrogen  chloride  a  jar  of  chlorine  is  inverted  over  a 


THE   HALIDES  59 

saturated  solution  of  ammonia  in  water  ;  oily  drops  are 
formed  which  settle  to  the  bottom  of  the  vessel  :  NH3.  Aq  + 
3C12  =  NC13  +  3HCl.Aq  ;  the  HC1  unites  with  ammonia, 
forming  ammonium  chloride. 

Endothermic  Combination.  —  This  body  is  fearfully 
explosive,  for  its  formation  is  attended  by  great  absorption 
of  heat  ;  but  during  its  formation  the  reagents  do  not  grow 
cold  ;  for  the  formation  of  ammonium  chloride  is  a  highly 
exothermic  reaction,  and  the  amount  of  heat  evolved  by 
its  formation  is  greater  than  that  of  the  equivalent  amount 
of  chloride  of  nitrogen  ;  hence  the  change  as  a  whole  is 
accompanied  by  evolution  of  heat.  It  is  thus  that  endo- 
thermic  compounds  are  usually  formed  :  by  virtue  of  a 
simultaneous  action  in  which  heat  is  evolved.  The  slightest 
shock  causes  the  decomposition  of  such  endothermic  bodies  ; 
if  one  single  molecule  is  decomposed,  it  evolves  heat  and 
brings  about  the  decomposition  of  its  neighbours  ;  and  as  all 
the  molecules  are  in  close  proximity  to  each  other,  and  as 
the  products,  nitrogen  and  chlorine,  are  both  gases,  and  are, 
moreover,  much  raised  in  temperature  by  being  set  free,  the 
decomposition  is  accompanied  by  sudden  and  enormous  ex- 
pansion. Nitrogen  iodide,  prepared  by  adding  a  solution 
of  iodine  to  aqueous  ammonia,  is  a  black  solid  of  the 
formula  NI3.NH3  ;  it  is  also  explosive. 

The  fluorides  of  boron  and  silicon  are  both  produced 
by  the  action  of  a  strong  solution  of  hydrofluoric  acid  on  the 
oxides  ;  but  it  is  necessary  to  have  some  agent  present 
to  withdraw  water,  such  as  concentrated  sulphuric  acid. 
These  compounds  are  both  gaseous.  Their  formation  is 
shown  by  the  equations:  B2O3  +  6HF  =  2BF3  +  3H2O  ; 
SiO2  +  4HF  =  SiF4+  2H3O.  If  the  water  is  not  with- 
drawn, combination  ensues  between  the  fluoride  and  hydrogen 
fluoride,  with  formation  of  HBF4  or  H9SiF6,  named  re- 
spectively hydroborofluoric,  and  hydrosilicifluoric  acids 
thus: 


2H2SiF6  +  H2SiO3.      These  compounds  ionise  into  H- 


60  MODERN   CHEMISTRY 

ions,  and  the  complex  ions  BF4  and  SiFfi  ;  and  many  salts 
are  known  in  which  metals  replace  the  hydrogen.  They 
are  similar  in  kind  to  potassium  aurichloride. 

The  other  halides  of  boron  and  silicon,  and  also  of 
phosphorus,  sulphur,  selenium,  tellurium,  and  iodine, 
react  at  once  with  water,  forming  hydrogen  halide  and  an 
acid.  The  equations  are  as  follows  :  — 

BCl3+3H9O.Aq       =    B(OH)3.Aq+3HCl.Aq; 

SiCl4+3H;O.Aq     -  O=Si(OH)9  +  4HCJ.Aq; 

PCJ3+3H9O.Aq       =   P(OH)3.Aq+3HCl.Aq; 

4H;O.Aq      =  0=P(OH)3.Aq+5HCl.Aq; 
2  +  2H0O.Aq  =  O=S(OH)2.Aq 

" 


9O.Aq:=  O=Te(OH)2.Aq  +  4HCl.Aq 

+  Te; 
+  3H9O.Aq      =  O=S(OH)2.Aq  +  4HCl.Aq; 

H2O.Aq     =  3HIO3.Aq+i5HCl.Aq  +  I2. 


It  is  to  be  noticed  that  where  a  hydroxy-compound 
corresponding  to  the  halide  is  capable  of  existence,  it  is 
formed  ;  if  not,  excess  of  the  element  is  set  free.  Hence 
none  of  these  halides  can  be  prepared  by  acting  on  the 
hydroxide  with  a  halogen  acid  ;  they  are  all  made  either 
by  the  direct  action  of  the  halogen  on  the  element,  or  by 
what  comes  to  the  same  thing,  the  action  of  the  halogen  on 
a  strongly  heated  mixture  of  the  oxide  of  the  element  with 
carbon.  Boron,  silicon,  and  phosphorous  chlorides  are  vola- 
tile liquids  ;  they  fume  in  the  air  owing  to  their  action  on 
the  water-vapour.  S9C12  is  a  yellow  liquid  ;  when  saturated 
with  chlorine  at  a  low  temperature,  SC19  and  SC14  are 
successively  formed  ;  but  on  rise  of  temperature  they  dis- 
sociate into  the  lower  chloride.  IC1  is  a  black  solid, 
converted  by  excess  of  chlorine  at  a  low  temperature 
into  IC13,  a  yellow  solid,  which  easily  dissociates  into 
IC1  and  C19  ;  and  PC15  is  a  pale  yellow  solid,  volatile  at 
a  high  temperature  in  a  perfectly  dry  atmosphere  without 


THE   HALIDES  61 

dissociation,  but  resolved  by  the  least  trace  of  moisture  into 
PC13  and  C12. 

Valency  of  Elements. — We  may  remark  here  the 
gradual  increase  of  valency  as  we  pass  from  left  to  right  in 
the  periodic  table.  Lithium  is  a  monad,  with  its  congeners  ; 
the  elements  of  the  beryllium  group  are  dyads ;  boron  a 
triad ;  carbon  a  tetrad  ;  phosphorus  acts  as  pentad  as  well 
as  triad ;  sulphur,  as  a  pseudo-monad,  a  dyad,  and  a  tetrad  ; 
and  Moissan  has  lately  shown  that  sulphur  burns  in  fluorine, 
forming  a  very  stable  hexafluoride,  SFC  ;  while  iodine  forms 
a  monochloride  and  a  trichloride,  and  probably  also  a 
pentafluoride  and  a  heptafluoride. 

Passing  back  to  the  boron  group,  if  it  is  desired  to  form 
anhydrous  chloride,  it  is  necessary  either  to  heat  the  element, 
or  its  oxide  mixed  with  charcoal,  in  a  current  of  chlorine, 
or,  except  in  the  case  of  boron,  to  prepare  a  double  salt  of 
the  chloride  with  ammonium  chloride,  and  to  volatilise  the 
latter  after  driving  off  the  water ;  the  aqueous  chlorides 
are  formed  by  dissolving  the  oxides  or  hydroxides  in 
hydrochloric  acid.  Thallium  forms  monohalides,  sparingly 
soluble  in  cold  water,  and  thereby  attaches  itself  to  the 
copper  group. 

Almost  the  same  remarks  apply  to  the  elements  of  the 
carbon  group ;  solutions  of  the  chlorides,  with  exception 
of  those  of  carbon  and  silicon,  are  obtained  from  the 
element  and  hydrochloric  acid  or  from  the  hydroxide,  and 
they  cannot  be  dried  without  reacting  wholly  or  partially 
with  water.  For  instance,  titanium  chloride,  on  careful 
addition  of  water,  can  become  ClTi(OH)3,  Cl2Ti(OH)2, 
ClgTi(OH),  all  of  which  are  intermediate  products  between 
the  tetrachloride  and  the  tetrahydroxide ;  such  compounds 
are  termed  "basic  chlorides."  Anhydrous  stannic  chloride 
is  a  fuming  liquid,  formed  by  the  distillation  of  a  mixture  of 
the  metal  with  mercuric  chloride  or  by  heating  the  metal 
in  a  stream  of  chlorine.  Lead  tetrachloride  is  a  very 
unstable  liquid,  formed  from  the  tetracetate,  Pb(C2H3O2)4, 
by  converting  it  into  the  double  ammonium  salt  with  a 


62  MODERN   CHEMISTRY 

mixture  of  ammonium  chloride  and  concentrated  hydro- 
chloric acid;  this  salt,  (NH4)t>PbC]r>,  is  then  decomposed 
by  concentrated  sulphuric  acid,  when  the  tetrachloride 
separates  as  a  heavy  liquid.  It  at  once  decomposes  into 
PbCl2  +  C10  on  warming ;  hence  PbO2,  when  warmed 
with  hydrochloric  acid,  undergoes  the  change:  PbO,-t- 
4HC1.  Aq  -  PbCl,  +  Aq  +  C12. 

Tin  and  lead  resemble  elements  of  the  zinc  group  in 
forming  dichlorides.  On  dissolving  tin  in  hydrochloric 
acid  the  dichloride  is  formed  ;  and  a  solution  of  the  tetra- 
chloride, when  exposed  to  the  action  of  nascent  hydrogen, 
yields  the  lower  chloride.  This  action  may  be  thus  for- 
mulated :—  S  n  C14.  Aq  +  2H  =  SnCl2.  Aq  +  HC1.  Aq. 
Stannous  chloride  is  a  white,  soluble  salt,  crystallising  with 
water  of  crystallisation.  Lead  dichloride,  on  the  other 
hand,  is  sparingly  soluble  in  cold  water  ;  it  is  formed  when 
a  soluble  lead  salt,  such  as  the  nitrate,  is  mixed  with  the 
solution  of  a  chloride:  Pb(NO3)2.Aq+  2NaCl.Aq  =  PbCl2 
+  2NaCl. Aq.  The  bromide  and  the  iodide  are  also 
sparingly  soluble,  and  are  similarly  produced. 

With  arsenic  and  the  remaining  members  of  that  group 
we  may  notice  the  same  characters  :  the  anhydrous  chlorides 
produced  by  the  action  of  chlorine  on  the  element,  or, 
when  it  is  not  available,  on  a  mixture  of  the  oxide  with 
carbon  at  a  red  heat ;  the  aqueous  solution  produced  by 
dissolving  the  oxide  or  hydroxide  in  hydrochloric  acid., 
Basic  chlorides  are  also  known,  e.g.  ClAsO,  CISbO,  and 
ClBiO,  from  the  trichlorides ;  and  OPC13,  and  OSbCl3,, 
from  the  pentachlorides,  on  reacting  with  a  small  amount 
of  water. 

Mass=Action. — The  action  of  mass,  that  is,  the  quan- 
tity of  a  compound  in  unit  volume,  is  well  illustrated  by  the 
action  of  water  on  antimonious  chloride.  A  solution  of  this 
salt  in  hydrochloric  acid  gives  a  precipitate  on  adding  water: 
SbCl3.nHCl.Aq  +  H2O  =  OSbCl  +  (n  +  2)HCl.Aq. 
Here  the  increase  in  the  number  of  molecules  of  water 


THE   HALIDES  63 

causes  the  precipitation  of  the  basic  chloride ;  on  adding 
more  hydrochloric  acid,  however,  so  as  to  increase  its 
active  mass,  the  reaction  is  reversed,  and  the  precipitate  re- 
dissolves  :  OSbCl+(n  +  2)HCl.Aq  =  SbCl3.Aq.nHCl-h 
Ht,O.  Above  a  certain  concentration  of  water  SbOCl  is 
stable ;  above  a  certain  concentration  of  hydrogen  chloride, 
SbCl3. 

The  higher  halides  of  molybdenum,  tungsten,  and 
uranium,  themselves  prepared  by  the  action  of  halogen  on 
the  element,  yield  tue  lower  halides  on  heating.  They  are 
volatile,  coloured  bodies,  soluble  in  water  ;  the  higher  ones 
are  decomposed  by  water. 

The  elements  chromium,  manganese,  iron,  cobalt, 
and  nickel,  although  not  all  belonging  to  the  same  series, 
show,  nevertheless,  a  gradation  of  properties.  The  dihalides 
of  all  are  known  in  the  dry  state ;  they  are  most  readily 
obtained  by  heating  the  metal  in  a  current  of  hydrogen 
halide,  if  required  anhydrous ;  or  if  in  solution  or  crystal- 
lised with  water,  by  dissolving  the  oxide  or  carbonate  in 
the  halogen  acid  and  evaporating  until  crystallisation  ensues. 
As  examples:  Fe  +  2HC1  =  FeCL  +  H.,0  ;  MnCO  -f 
2HBr.  Aq  -  MnBr2.  Aq  +  H2O  +  CO2. 

The  trihalides  are  best  made  by  heating  the  elements, 
in  a  current  of  halogen,  if  required  anhydrous  ;  if  in  solu- 
tion, by  dissolving  the  oxide  or  hydroxide  in  the  halogen 
acid.  The  trihalides  of  manganese  and  cobalt  are  very 
unstable ;  and  if  the  corresponding  oxides  be  treated  with 
halogen  acid,  a  portion  of  the  halogen  is  evolved,  thus : 
Fe9O3  +  6HCl.Aq  -  2FeCl3.Aq  +  3HQO  ;  Mn.,O8  +- 
6HC1.  Aq  -  2MnCl3Aq  +  sH2O.  But  MnCirAq  gradu- 
ally decomposes,  especially  if  temperature  is  raised,  thus  : 
2MnCl3.Aq=2MnCl2.Aq  +  Cl2.  And  if  MnO2  be  em- 
ployed, chlorine  is  evolved  from  the  outset :  2MnO2  -f- 
8HCLAq=2MnCl3.Aq  +  4H2O  +  CJ2;  the  MnCl3  de- 
composing further  on  standing  or  on  rise  of  temperature. 
With  Co2O3  a  transient  brown  coloration  is  noticeable  on. 
adding  hydrochloric  acid,  implying  the  momentary  forma- 


64  MODERN   CHEMISTRY 

tion  of  CoCl8.Aq  ;  but  it  is  at  once  resolved  into  CoCl.2.Aq 
and  free  chlorine. 

Oxidation  and  Reduction. — As  already  remarked, 
the  raising  of  the  valency  of  an  element  is  often  spoken  of 
as  "  oxidation  ;  "  the  reducing  of  the  valency,  as  "  reduc- 
tion." The  tendency  of  chromous  halides  to  transform 
into  chromic  compounds  is  so  great,  that  it  is  not  possible 
to  expose  them  to  air  without  the  change  taking  place, 
and  consequently  the  reduction  of  chromic  compounds  to 
chromous  is  a  difficult  operation.  But  with  iron,  both 
classes  of  compounds  have  nearly  equal  stability ;  hence 
oxidation  and  reduction  play  a  great  part  in  their  formation. 
The  action  of  nascent  hydrogen  from  any  source  reduces 
ferric  halide  into  ferrous:  FeCl3.Aq  +  H  =  FeCl9.Aq  + 
HC1.  Aq.  Similarly,  a  ferrous  halide,  in  presence  of  halogen 
acid  and  either  free  or  nascent  oxygen,  is  oxidised  to  a 
ferric  :  aFeCl,. Aq  +  2HC1.  Aq  +  O  =  2FeCl3.  Aq  +  H,O. 
Or  the  halogen  itself  may  be  used  to  effect  the  change  : 
2FeCl2.Aq  +  Q2  =  2FeCJ3.Aq.  On  evaporating  these 
solutions,  hydrolysis  takes  place  partially  ;  thus  ferric 
chloride  yields  compounds  of  a  basic  character,  such  as 
(OH)FeCl2,  (OH)2FeCl,  which  are  partly  hydroxide, 
partly  chloride.  This  statement  applies  to  the  halides  of  all 
these  metals. 

Colour  of  Ions. — The  triad  and  dyad  ions  in  the  case 
of  these  metals  exhibit  remarkable  differences  of  colour. 
Thus  chromous  ions  are  blue,  chromic,  green ;  basic  ferric 
ions  are  orange-yellow,  ferrous,  pale  green ;  manganic,  brown, 
manganous,  pale  pink  ;  cobaltous,  red,  and  nickelous,  grass- 
green.  Hence  a  change  in  the  ionic  charge  of  the  metallic 
ion  is  accompanied  by  a  striking  colour-change. 

The  halides  of  the  palladium  and  platinum  groups 
of  metals  closely  resemble  in  character  those  of  gold, 
which  have  already  been  described.  The  dihalides  of  the 
palladium  group  are  all  soluble,  save  PdI0,  which  is  pre- 
pared by  precipitation  with  potassium  iodide.  Nitro-hydro- 
chloric  acid  yields  the  higher  chloride  ;  it  remains  on  evapo- 


HALIDES   OF  COMPLEX   GROUPS  65 

ration.      These  form  with  chlorides  of  the  alkalies  double 
salts,  e.g.  RuCl3.2HCl,  RhCl3.2HCl,  and  PdCl4.2HCl; 

the  latter  are  probably  ionised  as  KK  and  PdCl6,  &c. 
Chlorine  also  acts  directly  on  red-hot  metals  of  the  platinum 
group,  forming  a  mixture  of  chlorides  ;  these,  on  heating,  lose 
chlorine,  giving  lower  chlorides.  Solutions  of  the  halides 
can  also  be  prepared  by  the  action  of  the  halogen  acid  on 
the  respective  oxides.  On  heating  to  a  high  temperature, 
all  these  halides  are  decomposed  into  the  metal  and  halogen. 
The  compounds  K2PtCl6  and  (NH4)2PtCl6  require  special 
mention ;  they  are  orange  salts,  nearly  insoluble  in  water, 
and  are  used  as  tests  for  potassium  and  ammonium,  and  also 
as  a  precipitant  in  estimating  these  ions.  Their  existence  is 
probably  to  be  ascribed  to  the  power  possessed  by  chlorine  of 
sometimes  acting  as  a  triad,  and  the  structural  formula  is  be- 
KCi=Cl\  /Cl  NH4C1=C1\  /Cl 


lievedtobe  >Pt<        and  >Pt<       . 

KC1= Cr       XC1        NH4Cl=C2i/      XC1 

Halides  of  certain  complex  groups  are  also  known. 
When  these  contain  oxygen  or  hydroxyl,  (OH),  they  are 
generally  termed  basic  salts  or  halo-acids  ;  they  will  be 
considered  later.  The  others  may  be  divided  into  two 
classes  :  those  like  ammonium  halides,  and  those  derived 
from  hydrocarbons. 

Ammonium  and  phosphonium  halides. — These  hal- 
ides, which  are  formed  by  direct  addition  of  the  hydrogen 
halide  to  ammonia  or  to  phosphine,  closely  resemble  in 
colour,  in  crystalline  form  (cubic),  and  in  reactions,  the 
halides  of  the  lithium  group  of  metals.  On  mixing  a  solution 
of  ammonia  and  hydrochloric  acid,  for  example,  the  combina- 
tion occurs:  NH3.Aq  +  HCl.Aq==NH4Cl.Aq ;  and  on 
evaporating  the  solution  to  dryness,  ammonium  chloride  is 
left  in  an  anhydrous  state.  From  the  conductivity  of 
ammonia  solution,  it  is  known  to  contain  a  certain  amount  of 
NH4OH  in  an  ionised  condition  ;  and  the  equation  may  be 

written:  NH4OH.Aq  +  HCLAq  =  NH4Cl.Aq  +  H2O. 

VOL.  II.  E 


66  MODERN   CHEMISTRY 

As  the  hydroxyl  ion  is  removed  from  the  solution  by  the  for- 
mation of  practically  non-ionised  water,  more  and  more  am- 
monium hydroxide  is  formed  to  maintain  equilibrium  between 
the  NH3.  Aq  and  the  NH4OH.  Aq  ;  and  the  whole  is  ulti- 
mately transformed.  The  rate  of  transformation,  however, 
is  a  very  rapid  one.  Combination  has  been  shown  not  to 
take  place  between  perfectly  dry  ammonia  and  dry  hydrogen 
chloride  ;  hence  it  does  not  seem  unlikely  that  ionisation 
may  occur,  either  in  the  gaseous  state,  or  more  probably  on 
the  surface  of  the  vessel  in  the  condensed  layer  of  moisture 
which  appears  always  to  adhere  to  all  solid  surfaces.  Once 
started,  combination  occurs  continuously  until  the  reaction  is 
complete.  Ordinarily  "dry"  ammonia,  however,  at  once 
gives  a  dense  cloud  with  hydrogen  chloride,  bromide,  or 
iodide.  Again,  perfectly  dry  ammonium  chloride  has  the 
vapour-density  26.25,  corresponding  to  the  molecular 
weight  (N=  I4  +  H4  =  4  +  C1  =  35.5)  =  53.5  ;  whereas,  if 
moist,  the  density  is  half  that  amount,  corresponding  with 
a  mixture  of  NH3  =  1 7  and  HC1  =  36.5.  These  compounds 
have  densities  of  8.5  and  18.25  respectively,  and  a  mix- 
ture in  equal  proportions  of  each  has  a  density  the  mean  of 
the  two,  viz.,  13.125.  It  appears  necessary  that  ionisation 

+ 

into  NH4  and  Cl  should  take  place  before  dissociation  into 
NH3  and  HC1  is  possible.  The  electrically  neutral  body 

+ 

NH4C1  can  volatilise  unchanged  ;  the  ions  NH4  and  Cl 
are  incapable  of  volatilisation  as  such,  and  in  volatilising 
unite  their  opposite  charges,  and  form  the  two  electrically 
neutral  compounds  HC1  and  NHg. 

PhospMne,  PH3,  also  unites  with  hydrogen  chloride, 
but  only  under  high  pressure,  at  the  ordinary  temperature. 
On  the  other  hand,  phosphonium  iodide,  PH4I,  is  pro- 
duced by  the  union  of  phosphine  with  hydrogen  iodide 
under  atmospheric  pressure  ;  it  forms  white,  cubical 
crystals,  which,  like  ammonium  chloride,  dissociate  when 
heated.  The  hydrides  of  arsenic  and  antimony  form  no 
such  compounds. 


PHOSPHINE  GROUPS  67 

It  must  be  assumed  that  these  compounds  are  formed 
with  change  of  valency  of  the  nitrogen  or  phosphorus  ;  the 
triad  becomes  pentad  ;  the  NmH3  becomes  H4NVC1.  On 
distilling  with  sodium  hydroxide  or  slaked  lime,  water  is 
formed,  and  the  element  is  reduced  to  its  original  triad  con- 
dition, thus:  NH4Cl.Aq  +  NaOH.Aq  =  NH4OH.Aq  + 

NaCLAq,  and  NH4OH.Aq  = NH3  +  H2O.Aq,  two 
electrically  neutral  bodies. 

Carbon  shows  no  such  tendency  to  change  valency. 
The  hydrocarbons  of  the  methane  series  are  "  saturated/' 
i.e.  they  have  no  tendency  to  take  up  any  other  element. 
Hence  halogen  must  replace  hydrogen.  This  can  be  done 
either  directly,  by  the  action  of  the  halogen  on  the  hydro- 
carbon, as,  for  instance,  CH4  +  C12  =  CH3C1  +  HC1  ;  or 
indirectly,  by  the  action  of  the  halogen  acid  on  the  hydr- 
oxide :  CH3OH  +  HC1  =  CH3C1  +  H2O.  Such  hydr- 
oxides are  termed  alcohols ;  that  derived  from  ethane, 
C2H6,  is  the  ordinary  anhydrous  alcohol  of  commerce  ;  its 
formula  is  C9H5OH,  and  the  corresponding  chloride  of 
ethyl  is  C0H,C1.  It  will  be  remembered  that  the  struc- 

H\      /H 

tural  formula  of  ethane   is   H-^C — QJ-H,  and    that    of 
H/          ^H 

H\          /H 
ethyl  chloride  is  H-^C— C^-C1.      There  is,  however,  a 

H/  \H 

difference  between  the  formation  of  ethyl  chloride,  for 
example,  and  of  sodium  chloride.  Whereas  sodium  chloride 
is  ionised  in  solution  in  water,  ethyl  chloride  is  insoluble, 
and  is  therefore  non-ionised.  Hence  the  action  is  a  slow 
one  ;  the  alcohol  is  saturated  with  hydrogen  chloride, 
allowed  to  stand  for  some  hours,  and  distilled  ;  ethyl 
chloride,  being  volatile,  passes  over  ;  it  is  a  gas,  condensing 
at  about  12°  to  a  mobile  colourless  liquid.  It  is  probable 
that  the  hydrogen  chloride  is  ionised  in  solution  in  alcohol ; 
the  alcohol  is  also  possibly  ionised  to  a  minute  extent  ; 


68  MODERN   CHEMISTRY 

water  is  formed  by  the  union  of  the  hydrogen  and  hydroxyl 

+ 
ions,  and  non-ionised  ethyl  chloride  distils  over  :  C0H.OH 

+  HCl.Alc  =  H2O  +  C,H5Cl.  But  this  suggestion,  it 
must  be  admitted,  is  somewhat  speculative,  and  is  based 
only  on  analogy  with  reactions  of  a  more  familiar  nature. 

The  formation  of  some  of  the  halogen  compounds  of  the 
olefines,  and  of  hydrocarbons  of  the  acetylene  and  benzene 
series,  has  already  been  alluded  to  on  p.  48. 


CHAPTER   IV 

Hydroxides  and  Acids — "Insoluble  Substances" — 
Indicators— Preparation  of  Basic  Oxides— Pro- 
perties of  the  Basic  Oxides  and  Hydroxides — 
Sulphides  —  The  ' '  Solubility-Product ' '  —  Basic 
Oxides  and  Hydroxides  of  Complex  Groups: 
Alcohols,  Aldehydes,  Ethers;  and  Sulphines, 
Amines  and  Phosphines. 

The  Oxides  and  Hydroxides,  Sulphides  and 
Hydrosulphides,  Selenides  and  Tellurides. — 

Owing  to  the  dyad  valency  of  oxygen,  sulphur,  selenium, 
and  tellurium,  compounds  of  these  elements  are  more 
numerous  than  those  of  the  halogens.  And  whereas  double 
halides  of  hydrogen  and  other  elements  are  not  numerous, 
being  confined  to  such  bodies  as  H2SiF6,  HBF4,  H.7PtCl6, 
and  a  few  others,  those  of  the  oxides  are  very  numerous, 
and  form  two  important  classes,  the  "  hydroxides "  and 
the  "acids." 

Hydroxides  and  Acids. — Members  of  both  these 
classes  may  be  regarded  as  hydroyxl,  that  is,  water  minus 
one  atom  of  hydrogen,  -OH,  in  combination  with  elements, 
but  they  differ  radically  in  that  the  true  hydroxides  ionise 

+      -  ++     - 

into  element  and  hydroxl,  thus:  NaOH.Aq,  Ca(OH)9.Aq, 
+  +  +     - 
Bi    (OH)3;    whereas   acids    ionise   into   hydrogen   and  a 

+    •  +    - 

negatively  charged  radical,  thus  :   HOCl.Aq,  HNO3.Aq, 
+    -   -  +    - 

H(HSOJ.Aq,  H0SO4.Aq,    and    many    others.       There 
69 


70  MODERN    CHEMISTRY 

are  certain  hydroxides  in  which  the  ionisation  may  take 
either  form  ;  such  compounds  are  said  to  be  either  "basic  " 
or  "  acid  "  according  to  circumstances  ;  thus,  aluminium 


hydroxide,   A1(OH)3,  is   basic;    with   hydrochloric    acid 

+  +  +   - 
it    reacts    in    the    following    manner:     Al(OH)3.Aq  + 


3HCl.Aq  =  Al  Cl3.Aq  +  3H2O;  on  the  other  hand,  when 
caustic  soda  is  presented  to  aluminium  hydroxide,  it  forms 
sodium  aluminate,  NaAlO2.Aq,  a  derivative  of  the  acid 
HAlOi;.Aq,  which  is  formed  from  A1(OH)3  by  loss  of 
water  :  "A1(OH)3  =  O=A1OH  +  H0O.  The  ions  in  the 

+ 
latter  case  are  H  and  A1O9,  and  the  reaction  takes  place 

between    HA1O2     and     NaOH,    thus:     HAlO2.Aq  + 

NaOH.Aq  =  NaAl62.Aq  +  H2O.  It  is  generally  the 
case  that  the  acids  are  derived  from  hydroxides  which 
have  lost  a  portion  of  their  hydrogen  as  water.  They 
are,  like  O=A1OH,  partly  oxide,  partly  hydroxide. 

"Insoluble  Substances."  —  The  hydroxides  are, 
with  some  exceptions,  generally  spoken  of  as  insoluble  in 
water.  The  word  "  soluble  "  is  a  relative  term  ;  it  is 
probable  that  very  few,  if  any,  substances  are  absolutely 
insoluble.  Silver  chloride  is  usually  regarded  as  wholly 
insoluble  in  water,  but  pure  water  shaken  up  with  that  salt 
acquires  increased  conductivity,  showing  that  some  chloride 
must  have  gone  into  solution.  In  one  of  the  equations 
given  above,  A1(OH)3  is  followed  by  "Aq,"  implying 
that  it  is  dissolved  and  ionised  in  solution.  This  method 
of  writing  is  perfectly  correct  for  the  portion  which  is  dis- 
solved, but  that  constitutes  only  a  very  minute  fraction  of 
the  whole.  What  is  dissolved,  however,  is  ionised  and 
enters  into  reaction,  and  when  it  has  been  removed,  as  in 
the  equation  given,  with  formation  of  practically  non-ionised 
water-molecules,  its  place  is  taken  by  more  :  equilibrium 
tends  to  establish  itself  between  the  dissolved  portion  and 


HYDROXIDES  AND  ACIDS  71 

the  portion  remaining  undissolved.  We  know  well  that  if 
excess  of  common  salt  be  placed  at  the  bottom  of  a  vessel 
of  water  it  will  not  all  dissolve,  but,  as  the  dissolved  portion 
diffuses  away  into  the  upper  layers  of  water,  its  place  is 
taken  by  fresh  salt,  which  dissolves,  until,  if  sufficient  time 
be  given,  the  whole  solution  becomes  saturated  with  salt. 
Similarly,  the  removal  of  the  aluminium — as  ions,  it  may 
be — and  of  the  hydroxyl  of  the  aluminium  hydroxide, 
A1(OH)3,  as  water,  on  treatment  with  an  acid,  causes  a 
fresh  portion  of  the  hydroxide  to  go  into  solution,  and  this 
continues  to  go  on  until  all  has  undergone  reaction. 

The  hydroxides  of  the  elements  may  be  classified  like 
the  halides ;  the  analogy  between  the  formulae  is  seen  on 
comparing  the  tables  on  pp.  72,  73,  with  those  on  p.  50. 

Oxygen  compounds  of  fluorine  are  wanting. 

[C1(OH)7],  [C1(OH)5],  [C1(OH)3],          Cl(OH). 

[OC1(OH)5],  [OC1(OH)3],          OCl(OH),  C12O. 

[02C1(OH)3]>  02C1(OH),  [C1203]. 

03C1(OH),  [C1205]. 
[C1207]. 

The  formulae  enclosed  in  brackets  are  of  unknown  sub- 
stances. The  whole  scheme  is  given  in  order  to  show  the 
gradual  loss  of  water  of  an  ideal  heptoxide. 

The  compounds  I(OH)6(ONa),  OI(OH)5,  O2I(OAg)3, 
and  O3I(OAg)  are  known,  corresponding  to  the  theoretical 
perhalic  acids.  Those  corresponding  to  the  halic  acids  are 
O2Br ( OH )  bromic  acid,  and  I ( OH ) 5  and  O2I (OH ) ,  iodic 
acids.  Br(ONa)  and  I(ONa),  named  respectively  hypo- 
bromite  and  hypoiodite  of  sodium,  are  also  known. 

It  may  be  noticed  that  the  formulae  of  some  of  the  com- 
pounds of  chromium  are  analogous  to  those  of  sulphur  and 
of  molybdenum  ;  other  compounds,  on  the  contrary,  show 
more  resemblance  to  those  of  iron.  While  manganese,  like 
chromium,  also  shows  analogy  with  iron,  it  too  forms 
O2Mn(OK)2,  like  O2S(OH)2  or  O 2Mo( OH )2,  termed 
potassium  manganate,  as  the  others  are  hydrogen  sulphate 
and  hydrogen  molybdate ;  and  also  MnO0,  analogous  to 


MODERN   CHEMISTRY 


0 

o 


:0 


:0    ..IS?: 


^     ^O 

ox    o o"oT 


UO      ^c 
OU      ""' 


ffl 

:0 


ffi  E 

i    iO    !  :    :0   ^ 

^  E^O1 

C?  (5h 


O  tn  O  'Oj2O  'O  'O  '  'OO 
^•^  in'  "o'c/^  r?  TT  v?  ~^r.£* 
W  W  fflffl 


^-q    Sr^o 
od'<    gdffi1 


:O 

P9 

OH 


•. 


ON 


:O    w 

OH 


fflOCQ 


ffi    :   „ 

a  '9, 


'2  '9,2 
j  5^ 


bjo  b/) 
SS 


:§0 


ffi        :    :a        :    :S 

&  '  '&>  '  '§9 

UU  WC/5  CQffi 


lu" 


OXIDES  AND   HYDROXIDES  73 

9,        °?  Q 

I-IH  HH  ,  -* 

c  ^  :         :        :         :      * 

O*     O     9     §  o*     O 

u     u     ^     ^  £>     D 


1 .  i  „  ^  1 1 .  i '  I 

^  9^o         ^    ^  o    5-  ^ 
duo^         oo^oo 


as  *  «  •:    « 

o   9.  »  d5  c?  '   c?  6s 

>*  >  9  j?  ^*  rt  cT 

O        O  >  Z  X  H  H 


£ 

1 1 

O         OH 


I  :  o   :  o  o: 


O  ^     «  OH 


£  :        :     £ 

o  o  o  o  o  •    o 

C  C  *O  T3  T3  bO 

N  N  U  O  O  X 


°        :       :     O     q, 

3  bO        tuO 

U  <        < 


74  MODERN   CHEMISTRY 

SO2  and  MoO2  ;  but  manganese  also  forms  O3Mn(OK), 
termed  potassium  permanganate,  which  is  analogous  in  formula 
as  well  as  in  crystalline  form  with  potassium  perchlorate, 
O3C1(OK).  It  is  convenient,  however,  also  to  include 
chromium  and  manganese  in  the  iron  group  of  elements. 

Cr(OH)3       Mn(OH)8     Fe(OH)3  Ni(OH)3  Co(OH)3 

OCr(OH)  OMn(OH)    OFe(OH) 

Cr2O3  Mn2O3          Fe2O3  Ni2O3  Co2O3 

Cr(OH)2       Mn(OH)2     Fe(OH)o  Ni(OH)2  Co(OH)2 

CrO  MnO  FeO  NiO  CoO 

Elements  of  the  palladium  group  have  a  very  wide  range 
of  valency  ;  hence  they  form  a  large  group  of  compounds. 

OsO4  IrO3 

Rh03        02Ru(OK)2          ...         02Os(OH)2  CX>Ir(OK)2 

Rh(OH)4       Ru(OH)4     Pd(OH)4       Os(OH)4  Ir(OH)4  Pt(OH)4 

Rh02             Ru02           Pd02             Os02  Ir02         PtO2 
Rh(OH)3       Ru(OH)3 

Rh0O3            Ru2O3               ...              OsoO3  Ir2O3 

Pd(OH)2           ...  ...          Pt(OH)2 

RhO              RuO            PdO              OsO  IrO          PtO 

The  hydroxides  of  lithium,  sodium,  potassium, 
rubidium,  and  caesium  are  all  soluble  white  compounds, 
melting  to  colourless  liquids  at  a  red  heat.  They  do  not 
lose  water,  even  at  the  highest  temperatures,  hence  the 
oxides  cannot  be  prepared  from  them  ;  indeed,  the  oxides 
are  produced  only  by  the  action  of  the  metal  on  the  hydr- 
oxide, at  a  high  temperature  ;  for  instance,  2NaOH  + 
2Na  =  Na2O  +  H2.  They  are  white,  non-crystalline  sub- 
stances, combining  at  once  with  water  to  form  the  hydr- 
oxides Na2O  +  H2O  =  2NaOH.  The  hydroxides  are 
prepared  from  the  carbonates  by  boiling  a  solution  with 
slaked  lime  (calcium  hydroxide)  :  Na2CO3.Aq  + 
Ca(OH)2.Aq  =  2NaOH.Aq  +  CaCO3;  or  by  heating  to 
redness  a  mixture  of  the  carbonate  with  ferric  oxide,  when 
the  ferrite  is  formed  :  K2CO3  +  Fe2O3  -  2KFeO2  +  CO2. 
On  treatment  with  water,  potassium  ferrite  is  decomposed, 
thus:  KFeO2  +  2H2O.Aq  =  KOH.Aq  +  Fe(OH)3. 


INDICATORS  75 

In  either  case,  the  solution  of  hydroxide  is  evaporated  to 
dryness  in  an  iron  vessel  and  fused. 

These  hydroxides  are  said  to  be  basic,  for  they  are 
neutralised  by  acids,  forming  salts.  Thus,  with  hydro- 
chloric acid,  KOH.Aq  +  HCl.Aq  =  KCl.Aq  +  H20, 
the  point  of  neutralisation — that  is,  when  the  acid  and  base 
are  present  in  theoretical  quantity  to  form  the  salt  and  water 
— is  determined  by  the  addition  of  an  "  indicator." 

Indicators. — The  most  important  indicators  are  litmus, 
phenol-phthalein,  and  methyl-orange.  Litmus  is, a  weak 
acid,  red  in  colour,  the  salts  of  which  are  blue.  When 
dissolved  in  water,  the  molecule  is  hardly  at  all  ionised, 
hence  the  red  colour  of  the  acid  is  alone  visible.  If  a  base 
such  as  sodium  hydroxide  is  added,  which,  in  aqueous  solu- 

+ 

tion,  is  largely  ionised  into  Na.Aq  and  OH.Aq,  the 
hydroxyl  ions  combine  with  that  portion  of  the  hydrogen 
ions  of  the  litmus  acid  which  exist  in  solution  ;  when  these 
are  withdrawn,  more  hydrogen  ions  take  their  place,  and  the 
solution  acquires  the  colour  of  the  ion  of  the  litmus  acid, 
viz.,  blue.  Conversely,  if  an  acid  be  added  to  a  base  in 
which  the  blue  litmus  ions  are  present,  the  hydrogen  ions  of 
the  acid  combine  with  the  hydroxyl  ions  of  the  base,  forming 
water,  so  long  as  any  are  present ;  after  they  are  all  in 
combination  they  convert  the  ion  of  the  litmus  acid  into  the 
red  acid,  non-ionised,  and  there  is  a  marked  colour-change. 
As  the  colours  of  the  litmus  acid  and  of  its  ion  are  both 
very  bright,  the  presence  of  a  mere  trace  of  the  indicator 
suffices.  Phenol-phthalein,  like  litmus,  is  also  a  weak  acid, 
that  is,  it  is  hardly  ionised  at  all  in  dilute  solution  ;  the  acid 
is  colourless,  but  the  ions  are  pink,  hence  the  addition  of  a 
trace  of  free  alkali  causes  the  colourless  solution  to  become 
pink.  But  this  indicator  gives  results  only  with  strong  bases, 
like  the  hydroxides  of  the  alkalies  ;  with  ammonium  hydr- 
oxide, present  in  a  solution  of  ammonia  in  water,  it  is  not  a 
good  indicator,  for  NH4OH  is  too  weak  a  base,  i.e.  the 
hydroxyl  and  ammonium  ions  are  present  in  too  small  amount 


76  MODERN   CHEMISTRY 

to  liberate  the  ions  of  the  phenol-phthalei'n,  unless  much 
ammonium  hydroxide  is  present  in  solution.  Hence  the 
presence  of  a  trace  of  free  ammonium  hydroxide  is  not 
revealed  by  that  indicator.  Phenol-phthalei'n  is  therefore 
serviceable  only  with  strong  bases,  but  it  may  be  used  for 
weak  acids.  Methyl-orange,  on  the  other  hand,  is  a  com- 
paratively strong  acid  ;  with  a  weak  base  it  forms  the  ions 
of  a  salt,  and  it  may  therefore  be  used  for  weak  bases  like 
ammonium  hydroxide,  or  for  strong  bases  like  the  hydrox- 
ides of  the  alkali  metals  ;  but  it  is  too  strong  an  acid  to 
serve  well  as  an  indicator  of  excess  of  a  weak  acid,  such  as 
carbonic  or  acetic  acid.  Its  colour-change  is  from  orange 
to  orange-pink. 

Preparation  of  Basic  Oxides. — The  hydroxides  of 
the  metals  of  the  sodium  group,  as  already  mentioned,  do 
not  lose  water  on  heating,  and  the  oxides,  therefore,  cannot 
be  thus  obtained.  Neither  do  their  carbonates  lose  carbon 
dioxide,  nor  their  nitrates  oxides  of  nitrogen,  save  at  an  im- 
practicable temperature.  But  all  other  basic  oxides  may  be 
prepared  by  heating  the  hydroxides,  carbonates,  or  nitrates 
of  the  metals,  and  a  few  may  be  obtained  by  heating  the 
sulphates.  Calcium  and  strontium  oxides  are  generally 
prepared  from  the  carbonates,  which  are  found  as  minerals, 
named  limestone  and  strontianite  respectively.  The  opera- 
tion of  preparing  "  quicklime  "  or  calcium  oxide  is  techni- 
cally, but  wrongly,  called  "  burning."  Alternate  layers  of 
lime  and  coal  are  placed  in  a  tower  of  brick  or  stone, 
termed  a  limekiln  ;  the  coal  is  set  on  fire,  and  its  heat 
expels  the  carbon  dioxide  from  the  carbonate :  CaCO3  = 
CaO+CO9.  If  calcium  carbonate  be  heated  in  a  closed 
vessel,  however,  so  that  the  carbon  dioxide  does  not  escape, 
the  dissociation  proceeds  until  the  amount  of  carbon  dioxide 
in  the  vessel  has  reached  a  certain  proportion,  which  is  per- 
fectly definite  for  each  temperature,  or  until  the  carbon 
dioxide  has  attained  a  certain  "  concentration."  The  reaction 
then  stops.  But  if  the  carbon  dioxide  be  removed  as  it  is 
formed,  the  reaction  goes  on  to  the  end,  until  all  carbon 


BASIC   OXIDES  77 

dioxide  has  escaped.  The  draught  in  the  kiln  removes  the 
carbon  dioxide,  hence  the  product  is  calcium  oxide.  Stron- 
tium carbonate  is  causticised  in  the  same  way  as  limestone  ; 
but  the  temperature  for  witherite  (BaCO3)  is  inconveniently 
high  ;  baryta  is  consequently  prepared  by  heating  the  nitrate, 
Ba(NOg),,  ;  it  may  be  supposed  to  split  into  BaO  and 
N.,O5  ;  the  latter,  however,  decomposes  even  at  moderate 
temperatures  into  NO2  and  O  ;  hence  the  equation  is  : 
2Ba(NO3),=  2BaO  +  4NO2  +  O2.  These  oxides  are 
whitish-grey  solids,  volatile  at  the  temperature  of  the  elec- 
tric arc,  and  combining  with  water  with  great  rise  of  tem- 
perature to  form  hydroxides.  The  hydroxides  are  sol- 
uble in  water — barium  hydroxide  most,  calcium  least.  An 
aqueous  solution  of  the  former  deposits  crystals  of  a  hydrate, 
Ba(OH)2.8H2O. 

The  sparing  solubility  of  calcium  hydroxide  makes  it 
possible  to  precipitate  it  by  the  addition  of  caustic  alkali  to  a 
soluble  salt  of  calcium,  provided  too  much  water  is  not  pre- 
sent :  CaCl2.Aq  +  2NaOH.Aq  =  Ca  (OH),  +  aNaCl.Aq. 
Of  course,  a  saturated  solution  of  calcium  hydroxide  remains, 
hence  the  precipitation  is  not  complete.  This  plan  is  appli- 
cable to  the  preparation  of  all  hydroxides  which  are  insoluble 
in  water,  unless  they  dissolve  in  excess  of  the  caustic  alkali ; 
if  they  do,  they  are  said  to  display  "  acid  "  properties. 
Beryllium  and  magnesium  hydroxides  are  thus  precipitated  : 
MgCl2.Aq  +  2KOH.Aq  =  Mg(OH)2+2KCl.Aq.  The 
hydroxide  may  be  filtered  off  and  dried,  and  the  white  mass, 
on  ignition,  leaves  the  oxide  as  a  white  powder.  By  this 
means,  too,  the  hydroxides  of  copper  (cupric,  Cu(OH)2), 
silver,  AgOH,  zinc,  Zn(OH)2,  cadmium,  Cd(OH),, 
aluminium,  A1(OH)3,  scandium,  yttrium,  lanthanum. 
and  ytterbium,  gallium,  indium,  and  thallium,  with 
similar  formulae,  titanium,  zirconium,  thorium,  with 
formulas  OM(OH)2,  (where  M  stands  for  an  element  of 
that  group;  germanium,  tin  (stannous,  Sn(OH)2,  and 
stannic,  SnO2.nH,O),  lead  (plumbous,  Pb(OH)2),  bis- 
muthous,  Bi(OH)3,  chromic,  Cr(OH)3,  and  chfomous, 


78  MODERN   CHEMISTRY 

Cr(OH)2,  manganic  and  manganous,  ferric  and  ferrous, 
cobaltous  and  nickelous  :  in  short,  from  all  elements  which 
form  "  basic  "  hydroxides.  And  from  almost  all  these  the 
oxides  may  be  obtained  by  heating  the  hydrates  to  redness. 
Excess  of  the  precipitant,  however,  must  be  avoided  in  many 
cases,  for  some  of  these  hydroxides  display  acid  properties 
if  in  presence  of  excess  of  alkali.  Thus,  for  example,  if 
excess  of  sodium  hydroxide  or  potassium  hydroxide  be 
added  to  the  solution  of  a  soluble  salt  of  zinc,  such  as  the 
chloride,  nitrate,  or  sulphate,  the  first  change,  as  already 
shown,  is  the  precipitation  of  the  hydroxide  ;  but  on  additi  :>n 
of  excess  of  alkali,  the  precipitate  redissolves,  forming  the 

+     + 
compound  Zn(OK)9.Aq,  of  which  the  ions  are  K,  K,  and 

ZnO9  ;  this  compound  is  thrown  down  by  alcohol,  in  which 
it  is  insoluble.  It  is  generally  named  zincate  of  potassium. 
Cadmium  forms  a  similar  compound,  but  that  of  aluminium 
has  the  formula  OAl(OK)  ;  the  hydroxide,  A1(OH)3,  on 
losing  water  is  transformed  into  the  condensed  hydroxide, 
OAl(OH),  which  may  be  termed  aluminic  acid,  of  which 
the  hydrogen  atom  is  exchangeable  for  metals.  Stannous 
and  plumbous  hydroxides  dissolve  in  excess  of  alkali,  doubt- 
less forming  compounds  similar  to  that  of  zinc  ;  and  chromic 
hydroxide  is  soluble  in  cold  solution  of  caustic  alkali,  form- 
ing, no  doubt,  a  compound  analogous  to  that  of  aluminium  ; 
but  it  is  decomposed  on  warming,  with  reprecipitation  of  the 
hydroxide.  The  hydroxides  of  all  these  elements  may  also 
be  precipitated  by  a  solution  of  ammonium  hydroxide,  and 
some  of  them  are  redissolved  ;  but  the  compounds  formed 
are  of  a  different  nature  from  those  described  in  the  case  of 
zinc,  &c.,  and  will  be  afterwards  considered. 

Properties  of  the  Hydroxides. — As  regards  the 
properties  of  the  hydroxides,  that  of  copper  (cupric)  is  light 
blue,  and  of  silver,  brown  ;  chromic  hydroxide  is  grey- 
green,  and  chromous,  yellowish  ;  manganic,  brown,  and 
manganous,  very  pale  pink  ;  ferric,  rust  brown,  and  ferrous, 
white  when  pure,  but  usually  dirty  green  ;  cobaltous,  dingy 


PROPERTIES  OF   HYDROXIDES  79 

red,  and  nickelous,  grass-green.  The  others  are  all  white 
amorphous  bodies,  and  they  all  yield  oxides  on  heating. 
Cupric  oxide  is  black  ;  even  when  boiled  with  water  the 
hydroxide  loses  water  and  changes  colour.  Argentous 
oxide  is  brown  ;  when  heated  to  redness  it  loses  oxygen, 
leaving  a  residue  of  metallic  silver.  Zinc  oxide  is  yellow 
when  hot  and  white  when  cold ;  cadmium  oxide  is  a 
brown  powder  ;  the  oxides  of  aluminium,  scandium, 
yttrium,  lanthanum,  ytterbium,  gallium,  and  indium,  and  of 
titanium,  zirconium,  thorium,  germanium,  and  stannic  oxide 
are  white  powders  ;  thallium  oxide  is  a  yellow  powder  ;  tin 
monoxide  is  a  black  powder  ;  that  of  lead  (litharge,  massi- 
cot) is  a  yellow  substance,  fusible  at  a  red  heat ;  bismuth 
sesquioxide  is  a  yellowish  powder ;  chromic,  ferric,  and 
manganic  are  respectively  green,  rust-red,  and  brown ; 
chromous  oxide  is  unknown,  for  any  attempt  to  dry  it 
results  in  the  decomposition  of  water,  the  absorption  of  its 
oxygen  by  the  chromous  oxide  which  becomes  chromic 
oxide,  and  the  evolution  of  hydrogen.  Ferrous  hydroxide 
can  be  dried,  but  only  with  rigid  exclusion  of  air ;  it 
is  a  black  powder.  Manganous  oxide  is  greyish-green, 
cobaltous,  olive-green,  and  nickelous  also  greyish-green. 
Manganous  hydroxide  must  also  be  dried  in  absence 
of  air. 

These  hydroxides  and  oxides  are  named  bases.  There 
are  some  basic  oxides,  which  are  precipitated  by  adding  a 
hydroxide,  such  as  that  of  sodium,  to  a  soluble  salt,  and  to 
which  there  is  no  corresponding  hydroxide.  This  is  the 
case  with  the  oxides  of  mercury.  On  referring  to  the 
table  of  halides  on  p.  50,  it  will  be  seen  that  the  chloride 
of  mercury  has  the  formula  HgCl9.  This  compound, 
commonly  called  corrosive  sublimate,  when  treated  in  solu- 
tion with  sodium  hydroxide,  gives  a  precipitate,  not  of 
hydroxide,  as  might  be  expected,  but  of  oxide  :  HgCl0.  Aq 
+  2NaOH.Aq  =  HgO  +  2NaCl.Aq  +  H2O.  Similarly, 
a  soluble  mercurous  salt,  such  as  mercurous  nitrate, 
Hg0(NO3)0,  on  treatment  with  an  alkali  gives  a  precipitate 


8o  MODERN   CHEMISTRY 

of  mercurous  oxide:  Hg2(NO3)0.Aq  +  2NaOH.Aq  = 
Hg2O  +  2NaNO3.Aq  +  H26.  These  are  cases  of  relative 
stability ;  for,  as  has  been  already  remarked,  on  boiling  a 
solution  from  which  cupric  hydroxide  has  been  precipitated, 
the  blue  hydroxide  is  changed  into  black  oxide ;  other 
hydroxides  lose  their  water  at  a  still  higher  temperature ; 
while  those  of  the  alkaline  metals  may  be  volatilised  without 
decomposing. 

Oxides  produced  by  Heating  Carbonates.— 
Most  of  the  basic  oxides  may  also  be  prepared  by  heating 
the  carbonates,  a  class  of  salts  afterwards  to  be  discussed. 
The  carbonates  of  the  alkali  metals,  however,  are  not  thus 
decomposed ;  like  their  hydroxides,  they  may  be  volatilised 
without  decomposition.  But  all  other  carbonates  are  de- 
composed by  exposure  to  a  red  heat.  The  process  has 
already  been  described  as  a  method  of  manufacturing  quick- 
lime. Most  carbonates,  however,  do  not  require  the  same 
high  temperature ;  a  dull  red  heat  suffices.  And  the 
oxides  do  not,  as  a  rule,  recombine  with  the  carbon  dioxide 
expelled,  as  does  lime ;  hence  there  is  no  danger  of  re-car- 
bonating  the  oxide. 

Oxides  produced  by  Heating  Nitrates. — The 
nitrates,  too,  of  nearly  all  the  basic  metals,  yield  the  respec- 
tive oxides  when  they  are  heated  to  bright  redness.  The 
nitrates  of  the  alkali  metals  in  this  instance,  as  in  others,  do 
not  behave  in  this  way.  When  heated  they  lose  oxygen, 
but  only  at  a  very  high  temperature,  forming  the  nitrites,  a 
class  of  salts  afterwards  to  be  described.  Thus,  potassium 
nitrate  undergoes  the  decomposition  :  2KNO3  =  2KNO9  + 
O2.  The  product  of  heating  the  other  nitrates,  however,  is 
the  oxide,  while  a  mixture  of  oxides  of  nitrogen  is  evolved. 
This  may  be  supposed  to  take  place  in  two  stages  :  first, 
the  nitrate  may  be  imagined  to  decompose  into  the  oxide 
and  nitrogen  pentoxide,  thus  :  Zn(NO8)2  =  ZnO  +  N2O5  ; 
the  last  compound  is  very  easily  decomposed  by  heat,  and 
yields  a  lower  oxide  of  nitrogen  :  2N2O.  =  4NO2  +  O2  ; 
while  if  the  temperature  is  over  600°,  which  is  usually 


SULPHIDES  AND   HYDROSULPHIDES       81 

exceeded  in  decomposing  the  nitrates,  the  nitric  peroxide  is 
partly  further  decomposed  into  nitric  oxide  and  oxygen  : 
2NO2  =  2NO  +  O2.  The  products,  therefore,  are  NO2, 
NO,  and  O2. 

A  metal  which  forms  two  oxides,  one  containing  more 
oxygen  than  the  other,  if  the  nitrate  of  the  lower  oxide  is 
heated,  yields  the  higher  oxide.  Cases  of  this  are  mercury, 
tin,  and  iron.  Mercurous  nitrate,  carefully  heated,  gives, 
not  mercurous  oxide,  Hg9O,  but  mercuric  oxide,  HgO  : 
HgNO3  -  HgO  +  NO2 ;  similarly  Sn(NO3)2  yields  SnO2, 
and  not  SnO  ;  and  Fe(NO3)2,  Fe2O3,  and  not  FeO. 

Oxides  produced  by  Heating  Sulphates. — 
The  sulphates  require  a  higher  temperature  than  the  nitrates 
for  their  decomposition,  consequently  they  are  not  generally 
used  as  a  source  of  oxides.  But  the  equivalents  of  mag- 
nesium, zinc,  and  some  other  metals  have  been  determined 
by  estimating  the  weight  of  oxide  obtainable  on  heating  a 
weighed  amount  of  sulphate ;  and  ferrous  sulphate  has  been 
distilled  in  fireclay  retorts  for  many  years  past  at  Nord- 
hausen,  in  Saxony,  for  the  purpose  of  making  "  Nordhausen 
sulphuric  acid,"  H2S2OK,  and  red  oxide  of  iron,  Fe2O3, 
which,  made  in  this  way,  has  a  fine  colour,  and  is  used  as  a 
paint.  When  a  sulphate  is  heated,  the  gas  which  escapes 
is  not  entirely  SO3,  as  might  be  imagined  from  the 
equation  :  MgSO4  =  MgO  +  SO3  ;  the  high  temperature 
decomposes  most  of  the  sulphur  trioxide  into  the  dioxide, 
SO0,  and  oxygen ;  and  the  oxygen,  in  the  case  of  ferrous 
sulphate,  oxidises  the  FeO  into  Fe2O3. 

Sulphides  and  Hydrosulphides. — The  analogy 
between  the  elements  oxygen  and  sulphur  is  well  shown 
by  comparing  the  sulphides  of  the  elements  of  which  the 
oxides  have  been  described.  Elements  of  the  lithium 
group  form  both  hydrosulphides  and  sulphides ;  thus  we 
know  sodium  hydro  sulphide,  NaSH,  analogous  to  the 
hydroxide  NaOH,  and  sulphide,  similar  in  formula  to 
the  oxide  Na9O,  Na9S.  Hydrogen  sulphide  is  a 
weak  acid  ;  hence,  on  passing  hydrogen  sulphide  through 


82  MODERN   CHEMISTRY 

a  concentrated  solution  of  sodium  hydroxide  at  95°  until 
saturation  is  complete,  white  crystals  of  NaSH.2H2O 

+     - 
deposit   on   evaporation.      The   equation    is  :     NaOH.Aq 

+  HSH.Aq  =  NaSH.Aq  +  H,O.  On  mixing  the  solu- 
tion with  an  equivalent  quantity  of  sodium  hydroxide  and 

+ 
evaporating,    the    sulphide    is    produced  :     Na  SH  .  Aq  + 

+     -  +    -  - 

NaOH.Aq  =  Na2S.Aq  +  H2O.  Here  it  must  be  sup- 
posed that  the  hydrogen  of  the  hydrosulphide  is  present  as 
an  anion,  and  that  it  reacts  with  the  hydroxyl  of  the  caustic 
soda,  forming  water,  while  the  sodium  sulphide  remains  in 
solution  in  an  ionised  form,  and  can  be  recovered  on 
evaporation  in  crystals  with  9H2O.  Similar  compounds 
exist  with  potassium. 

Calcium,  strontium,  and  barium  also  form  hydro- 
sulphides  and  sulphides,  analogous  in  formula  to  the 
hydroxides  and  oxides.  They  are  similarly  prepared  to 
the  sodium  compounds,  but,  as  the  metals  are  dyads,  their 
formulas  are  M(SH)2  and  MS;  and  there  is  an  inter- 
mediate compound  between  the  hydroxide  and  hydro- 
sulphide,  having,  in  the  case  of  calcium,  the  formula 
HSCaOH.  They  are  also  soluble  in  water.  Magnesium, 
too,  forms  a  hydrosulphide,  probably  Mg(SH)2;  it  is 
prepared  by  passing  sulphuretted  hydrogen  into  water  in 
which  magnesium  oxide  is  suspended.  It  is  unlike  the 
hydrosulphides  of  the  alkalies,  for  while  they  do  not 
decompose  with  water,  it,  on  the  contrary,  when  its  solution 
is  heated  to  80°,  reacts  with  water,  yielding  hydroxide 
and  sulphuretted  hydrogen:  Mg(SH)2.Aq  +  2HOH  = 
Mg(OH)2  -f  2H2S.  The  probable  explanation  of  this 
change  is  that  water  is  not  wholly  non-ionised,  but  that 
there  are  present  some  hydrogen  ions  ;  these  are  not  so 
inconsiderable  in  number,  compared  with  those  of  the  weak 
acid  H2S ;  on  raising  temperature,  a  certain  amount  of 
hydrogen  sulphide  is  liberated,  and,  being  volatile,  it  escapes, 


THE  SOLUBILITY-PRODUCT  83 

and  is  no  longer  present  to  act  on  the  magnesium  hydroxide 
and  reconvert  it  into  sulphide. 

Sulphides  of  boron,  aluminium,  chromium,  and 
silicon  are  at  once  decomposed  by  water,  and  cannot, 
therefore,  be  produced  in  aqueous  solution.  They  are 
white  substances  formed  by  heating  the  elements  to  a  high 
temperature  in  a  current  of  sulphur  vapour. 

The  sulphides  of  copper,  silver,  gold,  cadmium, 
mercury,  indium,  thallium,  tin,  lead,  arsenic,  anti- 
mony, and  bismuth,  and  of  the  metals  of  the  palladium 
and  platinum  groups,  are  all  insoluble  in  water,  or,  to  be 
more  accurate,  very  sparingly  soluble.  They  form  no 
hydrosulphides.  Hence  they  are  precipitated  from  soluble 
salts  of  these  metals  by  addition  of  sulphuretted  hydrogen  ; 
they  form  flocculent  precipitates,  usually  characterised 
by  striking  colours,  and  are  therefore  generally  used  as  a 
means  of  recognising  the  metal.  CuS,  Ag9S,  Au0S3, 
HgS,  T12S,  T12S3,  PbS,  PtS2,  and  the  other  sulphides 
of  the  platinum  group  of  metals  are  black  ;  CdS,  SnS2,  and 
As.,S3  are  yellow  ;  ln9S3,  SnS,  and  Bi9S3  are  brown,  and 
Sb9S3  is  orange.  These  sulphides  are  not  attacked  by  dilute 
acids.  On  the  other  hand,  the  sulphides  of  zinc,  manganese, 
iron,  cobalt,  and  nickel  are  not  precipitated  by  hydrogen 
sulphide,  but  they  are  thrown  down  by  a  soluble  sulphide 
or  hydrosulphide,  such  as  those  of  ammonium  or  sodium. 
They,  too,  form  flocculent  precipitates  ;  ZnS  is  white,  MnS 
pink,  and  FeS,  CoS,  and  NiS  are  black.  The  reason  of 
the  difference  in  the  behaviour  of  the  two  classes  of  sulphides 
is  an  interesting  one,  and  will  be  now  explained. 

Solubility** Product. — It  has  already  been  mentioned 
on  p.  14  that  the  rate  of  chemical  change  depends  on  the 
amount  of  each  of  the  reacting  substances  present  in  unit 
volume.  This  last  is  generally  termed  the  "  concentration  " 
of  these  substances,  for  the  more  concentrated  the  solution 
the  greater  the  mass  present  in  unit  volume.  Now,  if  two 

+ 
kinds  of  ions,  such  as  Na  and  Cl,  are  present  in  solution, 


84  MODERN   CHEMISTRY 

necessarily  in  equal  numbers,  the  solution  will  also  contain 
a  certain  number  of  molecules  of  non-ionised  NaCl,  formed 
by  their  union,  and  the  relative  number  of  ions  and  mole- 
cules will  depend  on  the  concentration ;  the  number  of  ions 
in  proportion  to  the  number  of  non-ionised  molecules  will 
be  greater,  the  greater  the  dilution.  For  each  dilutk 
(and  for  each  temperature)  a  state  of  balance  will  result; 
the  position  of  this  equilibrium  will  depend  on  the  relative 
rate  at  which  ionisation  and  union  of  ions  to  form  mole- 
cules go  on  ;  if  ionisation  takes  place  twice  as  quickly  as 
combinations  of  ions  to  form  molecules,  then  two-thirds 
of  the  dissolved  substance  will  exist  as  ions,  the  remain- 
ing third  being  non-ionised  molecules.  If  the  solution  is 
made  more  concentrated  by  evaporation,  the  conditions  are 
changed,  and  the  rate  of  ionisation  is  reduced  compared 
with  the  rate  of  union  of  ions  with  each  other.  Suppose 
that  concentration  be  pushed  so  far  that  solid  salt  separates 
out ;  the  limit  of  concentration  will  be  reached,  since  it  is 
now  impossible  to  alter  the  number  of  ions  and  of  molecules 
in  unit  volume  of  the  solution.  The  ratio  will  now  remain 
constant,  and  if  c  and  c  be  the  concentrations  of  the  ions 
(and  they  are,  of  course,  equal),  and  if  C  be  that  of  the 
non-ionised  molecules,  then  c.c  =  LC9  k  being  a  factor  ex- 
pressing the  relative  proportions  of  the  non-ionised  mole- 
cules. If  k  is  very  small,  then  there  are  many  molecules 
and  few  ions  present ;  if,  on  the  contrary,  k  is  large,  the 
ions  are  numerous  and  the  molecules  few.  The  expression 
LC  is  termed  the  "solubility-product." 

To  take  a  specific  case : — A  solution  of  ammonia  in 
water  consists  partly  of  the  ions  NH4  and  OH,  and 
partly  of  non-ionised  molecules  of  NH4OH  ;  it  is  a 
weak  base — that  is,  the  number  of  non-ionised  molecules 
is  much  greater  than  that  of  the  ions.  In  a  solution  con- 
taining 1.7  grams  of  ammonia  per  litre  (one- tenth  normal 
solution),  only  1.5  per  cent,  of  the  total  number  of  mole- 
cules exist  in  the  ionic  state.  Hence  a  solution  of  ammonia, 
unlike  one  of  caustic  soda  or  potash,  gives  no  precipitate 


INSOLUBILITY  OF  SULPHIDES  85 

of  hydroxide  when  added  to  a  solution  of  salts  of  the 
relatively  strong  bases,  such  as  calcium,  strontium,  or 
barium  chlorides.  With  salts  of  the  weaker  base  magnesia, 
however,  ammonia  produces  a  precipitate  of  magnesium 
hydroxide.  It  is  possible  still  further  to  reduce  the  ion- 
isation  of  ammonia  solution  ;  this  can  be  done  by  the 
addition  of  an  ammonium  salt,  such  as  the  chloride,  which, 
like  most  such  salts,  is  highly  ionised.  The  reason  is,  that 

+ 

while  (concentration  of  NH4)  x  (concentration  of  OH)  = 
k  x  (concentration  of  NH4OH),  if  more  ammonium  ions  be 
added,  the  number  of  hydroxl  ions  will  diminish  by  union 
with  NH4  ions,  forming  non-ionised  ammonium  hydroxide, 
because  the  increase  of  the  number  of  ammonium  ions  will 
increase  the  value  of  the  product  on  the  left-hand  side  of  the 
equation,  and  in  order  that  it  may  balance  that  of  the  right, 
the  relative  number  of  molecules  of  NH4OH  must  be  in- 
creased ;  and  we  may  see  that  if  ammonium  chloride  is  added 
to  a  solution  of  magnesium  chloride,  ammonia  solution  will 
no  longer  produce  a  precipitate  of  magnesium  hydroxide ; 
the  ammonia  is  too  weak  a  base,  that  is,  it  contains  too  few 
hydroxyl  ions,  which  are  the  reason  of  its  basic  nature. 

Let  us  now  return  to  the  consideration  of  the  insolubility  of 
sulphides  of  the  copper  group  in  acids  and  the  solubility  of  such 
sulphides  as  that  of  zinc.  No  substance,  as  has  been  before 
remarked,  is  wholly  insoluble  in  water  ;  zinc  sulphide,  how- 
ever, belongs  to  the  very  sparingly  soluble  compounds. 

+  + 

Hence  the  product  r(Zn)  xr'(S)  has  a  very  small  value, 
for  it  is  equal  to  >£.£(ZnS),  which  must  necessarily  be  very 
small,  seeing  that  the  compound  is  so  sparingly  soluble. 

+     + 

Now,  the  ions  of  H2S  are  H,  H,  and  S  ;  but  though  the 
ionisation  is  very  small,  hydrogen  sulphide  being  a  very 
weak  acid,  they  are  yet  sufficient  to  reach  the  value  of 
the  very  small  solubility-product  ^.C'(ZnS).  If,  however, 

the  concentration  of  the  S-ions  is   still   further  diminished 


86  MODERN   CHEMISTRY 

+ 

by  addition   of  some  compound   rich  in   H-ions,  such  as 
+  -  +  + 

HCl.Aq,  then  the  product  r(Zn)  xc(  S  )  will  be  less 
than  >£.£(ZnS),  and  there  will  be  no  precipitate  ;  or  if 
hydrochloric  acid  be  added  to  precipitated  zinc  sulphide, 
it  will  be  dissolved.  On  the  other  hand,  the  addition  of 
acetic  acid,  a  weak  acid,  and  poor  in  hydrogen  ions,  does 
not  bring  about  solution  of  zinc  sulphide  ;  indeed,  the  pre- 
cipitation of  zinc  from  a  solution  of  its  acetate  by  hydrogen 
sulphide  is  almost  complete. 

The  solubility-product  of  copper  sulphide,  and  of  the 
other  sulphides  which  are  not  soluble  in  dilute  acids,  is 
still  less  ;  hence  hydrogen  sulphide  precipitates  them  from 

acid  solution,  for  the  concentration  of  the  S-ions  of  the 
hydrogen  sulphide  may  be  very  much  diminished  without 

+  + 

the  product  r(Cu)  x  c  (  S  )  becoming  less  than  ^.£(CuS), 
for  CuS  is  still  less  soluble  in  water  than  ZnS. 

Oxides  and  Hydroxides  of  Complex  Groups. 
— The  oxides  and  hydroxides  of  complex  groups  show 
analogy  in  their  formulae,  and  often  in  their  methods  of 
preparation  with  the  basic  oxides  and  hydroxides.  A  few 
instances  of  these  will  now  be  given. 

Ammonia  (see  p.  42)  is  very  soluble  in  water  ;  at  the 
ordinary  temperature,  no  less  than  800  volumes  of  the  gas 
dissolve  in  one  volume  of  water,  forming  a  very  pungently 
smelling  solution  named  liquor  ammonia.  This  solution  con- 
sists for  the  most  part  of  a  mixture  of  liquid  ammonia  with 
water  ;  it  probably  also  contains  ammonium  hydroxide, 
NH4OH,  and,  as  already  mentioned,  less  than  1.5  per  cent. 

+ 
of  the  ions  NH4  and  OH.      It  is,  therefore,  a  weak  base. 

Hydrazine,  N2H4,  also  forms  a  hydrate,  N2H5OH, 
a  fuming  liquid  with  slight  smell  (and  consequently  in  all 
probability  fairly  highly  ionised)  ;  it  boils  at  119°,  and  is 
very  corrosive,  attacking  wood,  cork,  and  even  glass.  It  has 
a  strong  reducing  action,  so  that  if  added  to  a  solution  of 


ALCOHOLS  87 

cupric  sulphate  which  contains  cupric  ions,  Cu,  it  gives  an 
immediate  precipitate  of  cuprous  oxide,  Cu2O,  nitrogen 
being  evolved.  Like  ammonia,  it  precipitates  such  hydr- 
oxides as  that  of  aluminium,  iron,  &c.  Hydroxylamine, 
NH0OH,  is  a  somewhat  similar  body,  produced  by  passing 
nitric  oxide,  NO  (see  p.  97),  through  a  mixture  of  granu- 
lated tin  and  hydrochloric  acid,  to  which  a  little  platinic 
chloride  has  been  added  ;  the  nascent  hydrogen  reduces 
the  nitric  oxide  to  hydroxylamine  ;  it  unites  with  the 
hydrochloric  acid,  forming  hydroxylamine  hydrochloride, 
NH3OHC1.  After  removal  of  the  tin  by  addition  of 
sodium  hydroxide  and  filtration,  the  solution  is  evaporated 
to  dryness  and  mixed  with  alcohol ;  hydroxylamine  hydro- 
chloride  dissolves,  while  sodium  chloride  remains.  A  solution 
of  the  base  may  be  obtained  by  addition  of  silver  hydroxide  : 
NHgOHCl. Aq  +  AgOH. Aq  =  AgCl  +  NH3OH. Aq.  If 
sodium  methoxide  (see  p.  88)  be  added  to  a  solution  of  the 
hydrochloride  in  methyl  alcohol,  the  base  is  liberated,  and 
can  be  separated  from  the  alcohol  by  fractional  distillation  ; 
it  is  a  volatile  white  solid.  This  compound  is  interesting, 
because  the  OH  group  is  under  no  circumstances  an  ion  ;  its 

solution  in  water  must  contain  ions  of  NH3OH  and  OH, 
since  it  reacts  like  ammonium  hydroxide. 

Alcohols. — The  hydroxides  of  the  hydrocarbon 
radicles  are,  as  mentioned  on  p.  67,  termed  alcohols.1 
Of  these  there  are  very  many,  but  a  few  only  will  be 
chosen  to  serve  as  examples :  methyl  alcohol,  CHgOH, 
ethyl  alcohol,  CH3— CHQOH,  as  types  of  monohydric 
alcohols,  which  may  be  taken  as  the  analogues  of  the 

CH2OH 
hydroxides   of   the   monad    metals ;    glycol,  ,    a 

CH2OH 
dihydric   alcohol,   may   be   likened    to   barium   hydroxide, 

1  A  special  class  of  such  hydroxides  derived  from  benzene,  C6H6, 
are  termed  phenols.  "Carbolic  acid,"  C6H3OH,  is  the  best  known 
of  these. 


88  MODERN   CHEMISTRY 


CH2OH 
Ba(OH)9;     and    glycerine     (glycerol),    CHOH  ,    is    a 

CH2OH 

trihydric  alcohol,  as  aluminium  hydroxide  is  a  trihydroxide. 
These  substances  differ  from  the  hydroxides,  however,  by 
their  being  non-electrolytes,  and  therefore  non-ionised. 
Or  perhaps  it  is  more  correct  to  say  that  their  conductivity 
is  of  the  same  order  of  magnitude,  but  less  in  value,  than 
that  of  pure  water.  The  corresponding  halides,  for  ex- 
ample, CH3C1,  C2H4C12,  and  C3H5C13,  are  also  regarded 
as  non-ionised  ;  they  are  practically  insoluble  in  water. 
Nevertheless,  methyl  chloride  has  been  transformed  into 
methyl  alcohol  by  heating  with  water  to  a  high  temperature 
in  a  sealed  tube  under  pressure — CH3C1  +  HOH  = 
CH3OH  +  HC1 ;  and  the  others,  but  preferably  the  bro- 
mides, may  be  similarly  changed  into  hydroxides  by  heating 
with  silver  hydroxide,  or  with  silver  oxide  and  water  : 
CH2Br  CH2OH 

CHBr  +  sAgOH.Aq  =  CHOH  .Aq  +  3 AgBr.  Is  it 
CH2Br  CH2OH 

possible  that  at  a  higher  temperature  the  ionisation  is  suffi- 
cient (though  it  must  be  exceedingly  small)  to  produce  the 
interaction  ? 

The  metals  sodium  and  potassium  dissolve  in  the  alcohols, 
with  evolution  of  hydrogen,  forming  compounds  somewhat 
analogous  to  the  hydroxides  ;  instead  of  hydrogen,  however, 
they  contain  a  hydrocarbon  group  :  sodium  methoxide, 
for  example,  has  the  formula  Na(OCH3).  Such  sub- 
stances are  white  solids,  like  caustic  soda. 

Aldehydes. — The  alcohols,  if  oxidised  by  boiling 
them  with  chromic  acid,  yield  a  class  of  bodies  analogous 
to  the  oxides,  termed  aldehydes  :  CH3— CH2— OH  +  O 
=  (CH3  -  CH)"O  +  H2O.  It  will  be  noticed  that  ethane, 
CH3  —  CH3,  has  lost  two  hydrogen  atoms,  and  that  the 
residue,  CH3  —  CH0,  is  now  a  dyad  group,  capable  of  com- 
bination with  an  atom  of  dyad  oxygen.  The  aldehydes  are 
volatile  liquids,  with  strong  odour,  and  those  containing  few 


AMINES  AND   PHOSPHINES  89 

atoms  of  carbon  are  miscible  with  water.      They  form  easily 
decomposable  compounds  with  water,   which  are  di-hydr- 


oxides  ;  e.g.  ordinary  aldehyde  forms   CH3 

OH 

they  are  called  aldehydrols.  When  brought  into  contact 
with  solutions  from  which  hydrogen  is  being  evolved,  the 
aldehydrols  lose  oxygen,  and  are  converted  into  alcohols  : 

/OH 
CH3CH/        +  2H  =  CH3-CH2OH  +  H2O. 

The  alcohols  cannot  be  termed  basic  substances  ;  still,  it 
is  evident  that  they  show  analogy  with  the  true  bases  in 
many  respects. 

Amines  and  Phosphines.  —  Derivatives  of  nitrogen, 
phosphorus,  sulphur,  and  even  of  iodine  and  of  oxygen, 
containing  hydrocarbon  groups,  are  however  known, 
which  are  true  bases,  though  weak  ones.  If  ammonia 
in  alcoholic  solution  be  heated  with  excess  of  methyl 
iodide,  tetra-  methyl  -ammonium  iodide  is  formed  : 
NH3  +  4CH3I  =  N(CH3)4I  +  sHI.  This  iodide,  digested 
with  water  and  silver  hydroxide,  exchanges  iodine  for 
hydroxyl,  and  after  removal  of  the  silver  iodide  by  filtra- 
tion the  solution  may  be  evaporated  to  dryness.  The 
residue  is  a  white  solid,  of  the  formula  N(CH^)4OH  ; 
it  is  termed  tetra  -methyl-  ammonium  -  hy  dioxide  ;  in 
its  reactions  it  shows  great  analogy  with  caustic  potash, 
having  a  caustic  taste,  and  producing  precipitates  with 
the  usual  salts  of  the  metals.  In  solution  it  is  more 
ionised  than  ammonium  hydroxide,  though  less  than  that 
of  potassium. 

Phosphine,  as  remarked  on  p.  66,  combines  with 
hydrogen  iodide,  forming  a  salt,  PH4I,  phosphonium  iodide, 
resembling  ammonium  chloride.  But  as  it  is  decomposed 
by  water  into  phosphine,  PH3,  and  hydrogen  iodide,  an 
attempt  to  convert  it  into  phosphonium  hydroxide,  PH4OH, 
cannot  be  made.  Substituted  phosphonium  compounds, 


90  MODERN   CHEMISTRY 

however,  are  known,  in  which  a  hydrocarbon  radicle,  such 
as  methyl,  replaces  hydrogen.  Sodium  and  phosphorus 
combine  when  heated  together  under  an  oil  called  xylene, 
forming  PNa3  ;  this  body,  treated  with  methyl  iodide,  yields 
trimethyl  phosphine,  P(CH3)., ;  with  more  methyl  iodide 
P(CH3)4I  is  formed;  and  its  solution  in  water,  which  is 
not  decomposed  by  the  solvent,  yields  with  silver  hydroxide 
tetra-methyl-phosphonium  hydroxide,  P(CH3)4OH,  a 
base  resembling  the  corresponding  ammonium  compound. 

These  compounds  exist  owing  to  the  double  valency  of 
nitrogen  and  of  phosphorus,  which  can  function  either  as 
triad  or  pentad.  Double  valency  is  to  be  noticed  also  with 
oxygen  and  with  sulphur,  although  with  the  former  tetrad 
combinations  are  far  from  stable,  while  with  the  latter  both 
dyad  and  tetrad  compounds  can  be  formed. 

Ethers. — Oxide  of  methyl  and  oxide  of  ethyl,  which 
are  usually  named  methyl  and  ethyl  ethers,  are  formed  by 
mixing  solutions  in  alcohol  of  methyl  or  ethyl  iodide  with 
sodium  methoxide  or  ethoxide  :  CH3I.Alc  +  NaOCHg.  Ale 
=  Nal  +  HgCOCHg.  Ale.  The  ether  has  a  low  boiling- 
point,  and  can  be  separated  by  fractional  distillation  from 
the  alcohol  in  which  it  is  dissolved.  Methyl  ether  is  a 
gas;  ethyl  ether  a  volatile  liquid,  boiling  at  37°.  Such 
compounds  can  also  be  prepared  more  readily  by  distilling  a 
mixture  of  the  alcohol  with  sulphuric  acid,  which  yields 
HCH^SO4,  hydrogen  methyl  sulphate,  with  the  alcohol  : 
HCH3SO4  +  CH3OH  =  HgCOCHg  +  H2SO4.  Now, 
methyl  ether  and  hydrochloric  acid  combine  at  a  low 

CH3\      /H 
temperature,  yielding  /O\        >  but  it  is  impossible  to 

CH/     NCI 
replace  the  chlorine  by  hydroxyl. 

Similar  sulphur  compounds,  however,  are  stable.  Methyl 
sulphide,  produced  by  the  action  of  methyl  iodide  on  potas- 

CH3I     1C         KI     CH3, 

sium  sulphide,  +       J>S  —       +  J>S,  unites    with 

CHJ     K/      KI     CH/ 


ETHERS  91 


^ 
methyl  iodide,  forming  /S\  ?  a  compound  con- 

CH/  \I 

taining  tetrad   sulphur  ;    with    silver    hydroxide    it    yields 
the    corresponding    tri-methyl-sulphonium    hydroxide, 

CH3  CH3 

" 


,  a  compound  exhibiting  basic  properties. 
OH 

From  iodine,  too,  iodonium  compounds  have  been 
prepared,  in  which  the  iodine  functions  as  a  triad  ;  and  a 
hydroxide  with  basic  properties  is  known. 


CHAPTER   V 

Neutral  Oxides — Peroxides— Action  of  Nitric 
Acid  on  Metals;  on  Oxidisable  Substances 
— Complexity  of  Oxides — Spinels  and  Simi- 
lar Compounds. 

THE  properties  of  all  chemical  compounds  show  gradation ; 
and  there  is  a  slow  transition  from  basic  oxides  and  hydr- 
oxides, like  those  which  we  have  been  considering  in  the 
last  chapter,  to  acid  oxides  and  hydroxides.  The  transition 
takes  place  along  two  paths  ;  first,  there  are  some  oxides 
which  are  neither  basic  nor  acid ;  and  second,  a  number  of 
oxides  exist  which  are  either  basic  or  acid,  according  to 
circumstances.  We  shall  consider  first  the  neutral  oxides. 

Peroxides. — In  the  potassium  and  calcium  groups  of 
elements,  peroxides  are  known.  When  sodium  is  burned 
in  air  a  light  yellow  powder  is  formed,  sodium  dioxide, 
of  the  formula  Na2O2 ;  potassium  yields  a  tetroxide, 
K2O4.  Both  of  these  substances  react  with  water,  giving 
off  oxygen  ;  but  if  they  are  very  slowly  added  to  the  water, 
so  that  the  temperature  does  not  rise  much,  a  solution  is 
obtained.  The  corresponding  barium  compound  is  formed 
when  barium  monoxide  is  heated  under  pressure  in  air  (see 
p.  13).  On  addition  to  water  it  forms  a  hydrate,  probably 
Ba=O(OH)2.7H2O.  On  treatment  with  acid,  hydrogen 
dioxide,  H2O2,  is  formed ;  and  if  sulphuric  acid  be  added 
in  theoretical  amount  to  the  barium  dioxide,  nearly 
insoluble  barium  sulphate  is  formed,  along  with  a  fairly 
pure  solution  of  hydrogen  dioxide :  BaO=(OH)2.Aq 


NEUTRAL  OXIDES  93 

+  H2SO4. Aq  =  BaSO4  +  O=OH2.  Aq.  It  can  be  purified, 
and  indeed  obtained  anhydrous  by  distillation  under  very  low 
pressure.  It  then  forms  a  somewhat  viscous,  colourless 
liquid,  with  a  sharp  taste. 

There  is  some  doubt  as  to  the  constitution  of  hydrogen 
dioxide,  and  consequently  of  the  dioxides  from  which  it  is 
derived.  It  is  unlikely  that  barium  ever  acts  as  a  tetrad, 
and  much  more  probable  that  this  character  is  to  be  attri- 
buted to  oxygen  ;  hence  the  formula  of  its  dioxide  is  more 
likely  to  be  Ba=O=O,  than  O=Ba=-O  ;  and  consequently 
hydrogen  dioxide  has  more  probably  the  formula  O=OH2, 
than  HO=OH.  Indeed,  hydrogen  dioxide  is  possibly  a 
weak  acid,  since  the  hydrated  dioxides  of  calcium  and 
barium  are  precipitated  on  addition  of  concentrated  solu- 
tions of  hydrogen  dioxide  to  the  hydroxides  suspended  in 
water.  These  substances  have  all  bleaching  power,  for  they 
readily  part  with  their  second  atom  of  oxygen,  and  it  is 
capable  of  oxidising  coloured  insoluble  substances  to  colour- 
less soluble  ones. 

Neutral  Oxides,  Class  I. — The  next  neutral  oxides 
met  with  are  carbon  monoxide,  CO,  nitrous  oxide, 
N2O,  and  nitric  oxide,  NO.  These  are  all  gases,  but 
condense  at  low  temperatures  to  colourless  liquids,  and  at 
still  lower,  freeze  to  white  solids. 

Carbon  monoxide  is  prepared  by  burning  carbon  in  a 
supply  of  oxygen  insufficient  to  convert  it  into  the  dioxide  ; 
or  by  passing  the  dioxide  over  a  layer  of  carbon,  heated  to 
redness.  It  appears  that  the  monoxide  is  always  the  first 
product ;  for  if  moisture  be  excluded  during  the  combustion 
of  carbon  in  oxygen,  the  amount  of  dioxide  relatively  to  the 
monoxide  is  very  small ;  and  it  is  known  that  if  water-vapour 
be  absent,  carbon  monoxide  cannot  be  induced  to  explode  with 
oxygen.  If  even  the  minutest  amount  of  moisture  be  present, 
on  passing  a  spark  the  union  takes  place  with  explosion.  This 
phenomenon  is  not  easily  accounted  for  ;  it  is  readily  repre- 
sented by  the  equation  2CO  +H2O  +  O2=  2CO2  +  H2O. 
Can  it  be  that  at  the  very  low  pressure  of  the  water-vapour 


94  MODERN   CHEMISTRY 

+ 

a  trace  is  ionised  into  H  and  OH,  and  that  the  OH  furnishes 
the  oxygen  for  the  CO,  the  hydrogen  recombining  with 
oxygen  to  re-form  the  molecule  of  water  ?  For  it  has 
been  found  that  no  moisture  is  requisite  to  promote  the 
union  of  oxygen  and  hydrogen  if  these  gases  be  heated 
together.  Phosphorus  and  sulphur,  too,  show  reluctance  in 
uniting  with  oxygen,  in  absence  of  moisture.  In  ordinary 
moist  air,  carbon  monoxide  burns  with  a  blue  flame.  It  is 
nearly  insoluble  in  and  has  no  action  on  water. 

Other  methods  of  preparing  carbon  monoxide  are :  by 
withdrawing   the   elements  of  water  from  formic   acid   by 
adding   it   drop   by   drop   to  warm  concentrated   sulphuric 
O 

acid ; HC - OH  +  H2S04  =  CO  +  H2SO4.H2O  ;  by  heat- 
ing a  mixture  of  oxalic  acid  with  concentrated  sulphuric 

CO. OH 
acid ;     |  +  H9S04  =  CO  +  C02  +  H9SO4.H2O  ; 

CO.OH 

the  carbon  dioxide  is  separated  from  the  monoxide  by 
bubbling  the  mixture  of  gases  through  a  solution  of  caustic 
potash,  which  absorbs  the  dioxide,  allowing  the  monoxide 
to  pass  ;  and  lastly,  by  heating  a  mixture  of  potassium  ferro- 
cyanide  and  fairly  concentrated  sulphuric  acid  ;  K4Fe(CN)6 
+  6H.2S04  +  6H20  =  2K?S04  +  FeSO4  +  3  (NHJ,SO4 
+  6CO.  In  the  last  reaction,  it  may  be  taken  that  hydro- 
cyanic acid,  HCN,  is  first  liberated,  and  that  it  reacts 
with  water,  forming  ammonia  and  carbon  monoxide  :  HCN 
+  H2O  =  NH3  +  CO  ;  the  ammonia  subsequently  combines 
with  the  sulphuric  acid. 

If  carbon  monoxide  is  passed  over  metallic  nickel  or 
iron  in  a  fine  state  of  subdivision  produced  by  reducing 
their  oxides,  volatile  compounds  are  formed  of  the  formulas 
Ni(CO)4,  and  Fe(CO)5;  on  exposing  the  latter  to  light 
gold-coloured  crystals  are  formed,  of  the  formula  Fe2(CO)^. 
The  nickel  carbonyl  boils  at  43°,  and  the  iron  penta- 
carbonyl  at  103°;  di-ferro-hepta-carbonyl  decomposes 


NITROUS  OXIDE  95 

when  even  moderately  heated.  At  180°  these  compounds 
are  decomposed  into  metal  and  carbon  monoxide,  the  metal 
being  deposited  as  a  mirror  on  the  hot  surface. 

Nitrous  oxide,  N2O,  is  most  readily  prepared  by 
heating  ammonium  nitrate,  NH4NO3 ;  the  equation  is : 
NH4NO3-N2O  +  2H2O.  It  is  somewhat  soluble  in 
water,  and  is  best  colfected  by  downward  displacement. 
The  aqueous  solution  has  a  sweetish  taste  ;  and  the  gas,  if 
breathed,  produces  insensibility  ;  it  is  therefore  frequently 
employed  by  dentists  as  an  anaesthetic.  If  a  mixture  with 
air  is  respired,  it  produces  with  some  persons  a  state  of 
excitement,  which  has  procured  for  it  the  name  "  laughing- 
gas."  It  is  an  endothermic  compound,  and  if  submitted  to 
sudden  shock  it  explodes  with  violence.  It  may  be  sup- 
posed that  the  fulminate  used  to  explode  it  decomposes 
some  molecules  in  the  neighbourhood ;  these,  on  decompos- 
ing, evolve  heat,  and  decompose  their  neighbours,  and  the 
explosion  rapidly  travels  throughout  the  gas  ;  the  products 
are  nitrogen  and  oxygen.  A  candle  will  burn  in  nitrous 
oxide,  for  the  temperature  of  the  flame  is  sufficiently  high 
to  decompose  the  gas,  and  the  combustion  proceeds  as  in 
dilute  oxygen.  Although  nitrous  oxide  is  not  acted  on  by 
water  or  bases  it  has  claims  to  be  regarded  as  the  anhydride 
of  hyponitrous  acid,  from  a  solution  of  which  it  is  liberated 

N-OH     N, 
by  heat:     ||  -  li  \O+H9O.      As  neither  ammo- 

N-OH     N/ 

nium  nitrate  nor  hyponitrous  acid  can  be  reproduced  by 
bringing  together  nitrous  oxide  and  water,  its  production  by 
heating  one  of  these  compounds  is  termed  an  "  irreversible 
reaction." 

Action  of  Nitric  Acid  on  Metals. — The  product 
of  the  action  of  nitric  acid  on  metals  varies  according  to  the 
metal  acted  on,  the  concentration  of  the  acid,  and  the 
temperature.  The  acid  in  aqueous  solution  is  more  or  less 

-f 
ionised,  the  ions  being  H  and  NO3.      If  a  metal  of  which 


96  MODERN   CHEMISTRY 

the  ions  are  highly  electropositive  is  presented  to  these  ions 
of  nitric  acid  the  hydrogen  ions  impart  their  charge  to  the 
non-ionised  metal,  which  metal  enters  into  solution  as  ions, 
while  hydrogen  is  evolved.  This  is  the  case  when  nitric 
acid  acts  on  magnesium,  and  theoretically  also  on  aluminium, 
manganese,  zinc,  cadmium,  iron,  cobalt,  and  nickel,  for  all 
these  metals  in  the  ionic  state  have  higher  electro-affinity 
than  hydrogen,  and  that  in  the  order  given.  It  may  be 
termed  the  normal  action  of  acids  on  metals,  and  repre- 

+  + 

sented  thus  :  M  +  2H  =  M  +  H2.  But  along  with  this 
action  others  take  place  in  which  the  nitric  ion  is  "  re- 
duced "  or  deprived  of  oxygen.  Some  examples  of  this 
will  now  be  given. 

When  silver  is  attacked  by  nitric  acid,  nitric  peroxide, 
NO9,  is  produced,  and  partly  evolved  as  gas.      The  react- 

H        NO3 

ing    substances    are    Ag,    and    +   and  ;    one    of  the 

H        N03 

NO3  groups  loses  oxygen,  being  converted  into  electrically 

neutral  NO2  and  an  ion  of  oxygen,  O,  which  combines 
with  the  two  hydrogen  ions,  forming  water,  non-ionised, 
H2O.  But  this  leaves  a  negatively  charged  nitrate  group 
without  a  corresponding  positively  charged  partner ;  more- 
over, the  charge  of  the  decomposed  nitrate  group  is  still 
available.  An  atom  of  silver,  therefore,  goes  into  solution 
as  a  positively  charged  ion,  and  restores  electric  equilibrium 
in  the  solution.  With  less  concentrated  acid  the  nitrate  ion 
parts  with  two  atoms  of  oxygen,  requiring  three  negative 
electrons,  in  addition  to  the  one  originally  attached  to  the 

group  NO3 ;  to  effect  this  three  positive  electrons  must 
attach  themselves  to  three  atoms  of  silver,  which  then  go 

+ 
into  solution  as  ions,  hence  the  charge  is  :    3  Ag  +  4-H  + 

4NO3  =  NO  +  2H2O  +  3 Ag  +  3NO3,  the  balance  of  elec- 


OXIDES  OF  NITROGEN  97 

trie  charge  not  having  been  disturbed,  although  one  nega- 
tive and  one  positive  electron  have  disappeared.  With 
metals  yielding  kations  of  higher  potential,  the  reduction  of 
the  nitrate  ion  goes  still  farther  ;  nitrous  oxide,  N2O, 
nitrogen,  and  even  ammonia  may  be  produced,  in  relative 
amounts  depending  on  the  metal,  on  the  concentration,  and 
on  the  temperature.  It  may  be  taken  that  the  lower  the  tem- 
perature, the  less  the  concentration,  and  the  higher  the  metal 
stands  in  the  electro-negative  series,  the  greater  the  reduc- 

+ 
tion.      The  equations  are  :    qM"  +  loH  +  ioNO3  =  N2O 

i2NO   =  N 


2 

6H,0  +  5  M+  i  oN03  ;    4M"  +  i  oH  +  i  oNO3  =  NH4  + 
" 


.  All  these  changes  may  proceed 
simultaneously  ;  but  copper  and  moderately  strong  nitric 
acid  yields  fairly  pure  nitric  oxide  ;  if  more  concentrated 
acid  be  employed,  a  mixture  of  varying  proportions  of  nitric 
oxide  and  peroxide  are  evolved  ;  while  by  using  zinc  or 
magnesium  and  very  dilute  acid,  nitrous  oxide,  nitro- 
gen, hydrogen,  and  ammonium  nitrate  are  the  main 
products. 

Oxidation  by  means  of  Nitric  Acid.  —  Action  of 
the  same  nature  occurs  when  an  element  capable  of  chang- 
ing its  valency,  i.e.  the  number  of  electrons  associated  with 
its  ionised  atom,  is  treated  in  the  ionic  condition  with  nitric 

+  + 
acid.       For  example,   the  ferrous  ion,   Fe,   on   treatment 

+  +  + 
with  nitric  acid  at   100°  becomes  ferric,  Fe,  while  nitric 

+  +  + 

oxide  is  evolved  :   3  Fe  +  6R  +  4H  +  4NO3  =  NO  +  2H2O 

+  +  + 

+  3Fe+  3NO3  +  6R  ;  R  being  any  monovalent  anion. 
Such  operations  are  usually  spoken  of  as  "  oxidations  in 
the  wet  way/' 

Nitric  oxide  is  a  colourless  gas,  very  sparingly  soluble 
in  water  ;  on  bringing  it  into  contact  with  oxygen,  unless 

VOL.  II.  G 


98  MODERN   CHEMISTRY 

moisture  is  absolutely  excluded,  union  takes  place  to  form 
nitric  peroxide,  NO2,  along  with  a  trace  of  N2O3,  nitrous 
anhydride.  On  sufficiently  cooling  nitric  oxide  it  con- 
denses to  a  colourless  liquid,  and  at  a  still  lower  temperature 
it  forms  a  white  solid. 

Nitrous  anhydride,  strictly  speaking,  belongs  to  the  class 
of  acid-forming  oxides  ;  its  formula  is  N2O3,  When  nitric 
oxide  and  nitric  peroxide  are  brought  together,  only  a  minute 
quantity  of  N2O,}  is  formed  ;  that  is,  because  on  converting 
it  into  the  gaseous  state  it  decomposes  almost  completely 
into  these  products.  On  cooling  such  a  mixture,  however, 
a  blue  liquid  condenses,  which  has  the  formula  N9Og.  It 
will  be  afterwards  alluded  to. 

Nitric  peroxide,  as  usually  seen  mixed  with  air  at 
ordinary  temperatures,  is  an  orange-coloured  gas.  When 
pure  it  condenses  to  an  orange-red  liquid,  boiling  at  22° ; 
it  freezes  at  — 10°  to  a  colourless  solid.  The  liquid  has  a 
molecular  weight  corresponding  to  the  formula  N2O4,  and 
the  gas,  at  temperatures  not  much  exceeding  the  boiling- 
point,  consists  mainly  of  the  same  substance.  But  as  the 
temperature  rises  the  colour  grows  darker,  until,  at  140°,  it 
forms  a  blackish-red  gas,  consisting  wholly  of  NO2.  With 
progressive  increase  of  temperature  NO2  dissociates  in  its 
turn  into  NO  and  O2,  and  at  600°  the  change  is  complete. 
As  temperature  falls  the  action  is  reversed. 

Neutral  Oxides,  Class  II.  —  The  next  class  of 
oxides  comprises  those  which  may  be  termed  neutral, 
because  they  can  act  either  as  bases  or  as  acids,  according 
as  they  are  treated  with  an  acid  or  with  a  base.  Their 
hydroxides  may  be  comprised  in  the  same  class.  A  case 
of  this  kind  has  already  been  explained  on  p.  70 ;  it  is 
there  shown  that  aluminium  hydroxide,  when  treated  with 
acids,  yields  salts  of  aluminium,  while  with  bases  aluminates 
are  formed. 

Complexity. — It  appears  probable  that  such  oxides 
have  molecular  formulae  more  complex  than  those  usually 
ascribed  to  them;  for  instance,  aluminium  oxide  is  certainly 


NEUTRAL  OXIDES  99 

more  complex  than  is  implied  by  the  usual  formula  A19O3  ; 
it  may  be  A14O6  or  A16O9,  but  there  is  no  means  at  present 
of  determining  the  degree  of  complexity  of  the  molecule. 
The  argument  in  favour  of  this  view  is  the  very  high 
melting-points  and  boiling-points  of  such  oxides.  It  is  a 
well-known  fact  that  as  the  molecular  weight  of  compounds 
increases  the  boiling-point  rises.  Examples  to  illustrate 
this  are  best  drawn  from  carbon  compounds,  where  "  poly- 
merism"  is  not  infrequent ;  that  is,  where  compounds  exist 
having  the  same  percentage  composition  but  molecular 
formulas,  of  which  the  higher  ones  are  multiples  of  the 
lower  one.  We  are  acquainted  with  a  series  of  com- 
pounds of  carbon  and  hydrogen,  of  which  the  first  member 
is  ethylene,  C2H4  ;  bodies  of  the  formulae  C4Hg,  C6H12, 
C8H16,  C10H20,  &c.,  are  also  known  ;  and  the  boiling-point 
increases  with  the  molecular  weight.  Now,  the  chlorides 
of  the  elements  are,  as  a  rule,  easily  volatile,  and  have  low 
melting-points  ;  and  where  it  happens  that  both  chloride  and 
oxide  have  a  simple  molecular  formula,  as,  for  example, 
carbon  tetrachloride,  CC14,  and  carbon  dioxide,  CO9,  the 
chloride  has  always  a  higher  boiling-point  than  the  oxide. 
It  would  appear  to  follow,  therefore,  that  if  the  oxides  of 
the  metals  had  as  simple  molecular  formulae  as  the  chlorides 
they  would  show  more  volatility  than  the  latter.  As  this 
is  not  the  case,  the  presumption  is  that  the  oxides  possess 
more  complex  formulae  than  we  are  in  the  habit  of  ascribing 
to  them.  This  probability  will  be  dealt  with  as  occasion 
arises. 

Among  the  oxides  and  hydroxides  which  exhibit  the 
power  of  acting  both  as  acid  and  basic  compounds  are 
cupric  hydroxide,  Cu(OH)2,  which  dissolves  in  a  con- 
centrated solution  of  potassium  hydroxide  with  a  dark  blue 
colour ;  zinc  and  cadmium  hydroxides,  which  dissolve 
in  excess  of  alkali ;  sodium  zincate  has  been  separated  by 
addition  of  alcohol,  and  is  precipitated  in  white  needles  of 
the  formula  Na2ZnO2.8H2O;  and  aluminium  hydroxide, 
which  dissolves  in  alkali,  forming  an  aluminate,  MA1O2  ; 


ioo  MODERN   CHEMISTRY 

stannous  and  plumbous  hydroxides,  Sn(OH)2  and 
Pb(OH)2,  dissolve  in  alkalies,  forming  Compounds  no 
doubt  analogous  to  zincates.  Chromous,  ferrous,  manganous, 
cobaltous,  and  nickelous  hydroxides  are  not  thus  soluble. 
Chromic  hydroxide,  however,  is  soluble  in  soda,  probably 
forming  a  compound  like  sodium  aluminate ;  unlike  the 
latter,  chromium  hydroxide  is  thrown  down  on  boiling  the 
solution. 

But  such  compounds,  when  they  do  not  contain  sodium 
or  potassium,  are  often  insoluble  in  water,  and  then  they 
cannot  be  prepared  by  the  action  of  the  one  hydroxide  on 
the  other.  The  oxides  combine  when  heated  together  in 
the  dry  condition,  and  sometimes  when  the  compound 
formed  is  decomposed  by  water  (hydrolysed)  it  is  con- 
venient to  prepare  it  either  from  the  oxide  or  from  the 
carbonate. 

Spinels.  —  A  considerable  number  of  compounds, 
analogous  to  the  aluminates,  is  produced  in  this  way,  and 
many  of  them  are  found  in  nature  as  minerals.  To  this 
class  belong  the  "  spinels,"  so  called  because  one  of  their 
number,  the  native  aluminate  of  magnesium,  had  received 
this  name.  Viewed  as  a  combination  of  oxides,  such  com- 
pounds possess  the  general  formula  M2OrMO,  and  they 
can  be  prepared  by  heating  the  sesquioxide  (a  name  given 
to  oxides  when  the  proportion  between  the  metal  and  the 
oxygen  is  as  one  to  one  and  a  half,  or,  more  correctly,  as 
two  to  three)  with  the  monoxide.  The  spinels  all  crystal- 
lise in  regular  octahedra ;  they  are  therefore  said  to 
be  isomorphous  with  each  other.  Viewed  as  aluminates, 
they  may  be  written  M"(MO9)9  ;  compare  NaAlO.,. 
Among  them  are  true  spinel,  Mg(AlO2)2;  franklinite, 
Zn(FeO2)2;  chrysoberyl,  Be(AlO2)2;  and  chromite, 
or  "chrome-iron  ore/'  Fe(CrO2)2.  But  it  is  not  neces- 
sary that  the  metals  of  a  spinel  should  be  different  ones ; 
if  a  metal  is  capable  of  existing  in  two  forms,  e.g.  as  dyad 
and  triad,  it  may  form  a  similar  compound.  Such  are 
magnetite^  or  "magnetic  iron  ore/7  Fe"(Fe'"O2)2,  and 


SPINELS  •    •  101 

hausmanite,  Mn"(Mn'"C,)<,,  th^  lirst  atom-  of  .Iron  or 
manganese  being  dyad,  like  magnesium,  and  the  second 
triad,  like  aluminium. 

Reasoning  by  analogy,  it  would  appear  not  unlikely  that 
native  oxides,  such  as  alumina  (corundum,  ruby,  sapphire), 
or  iron  sesquioxide  (haematite),  may  be  in  reality  an 
aluminate  of  alumina,  A1(A1O0)3,  or  ferric  ferrite, 
Fe(FeO,)8. 

A  common  test  for  zinc  and  aluminium  is  to  heat 
together  before  the  blow-pipe  the  salt  suspected  to  contain 
the  metal  with  cobalt  nitrate  ;  it  is  probable  that  the  green 
colour  produced  by  zinc  is  due  to  the  formation  of  a  cobalt 
zincate,  Co(ZnO0),  and  the  blue  colour  shown  by  alumina 
to  a  similar  body,  Co(AlO2)2. 

When  lead  is  heated  to  redness  in  air  the  first  product 
of  its  oxidation  is  litharge,  PbO  ;  on  continuing  the  ap- 
plication of  heat,  at  a  carefully  regulated  temperature,  the 
yellow  litharge  becomes  red,  and  the  product  of  the  action 
is  minium  or  "  red  lead,"  PbgO4.  Now,  on  treating  red 
lead  with  dilute  nitric  acid,  lead  nitrate  dissolves,  while 
lead  dioxide,  hydrated,  remains  as  an  insoluble  residue. 
Red  lead,  therefore,  may  be  regarded  as  a  compound 
between  two  molecules  of  monoxide  and  one  of  dioxide, 
2  PbO  +  PbO2  ;  the  former  reacts  with  nitric  acid  forming 
the  nitrate,  while  the  latter  remains.  Now,  if  the  dioxide 
be  heated  with  caustic  potash  it  dissolves,  forming  potassium 
plumbate,  K.JPbO3  ;  and  red  lead  may  be  regarded  as  a 

/Pb"\     iv 
basic    plumbous    plumbate,    O<^  VPbOg)  ;    "basic," 

\pb"/ 

because  the  first  written  atoms  of  lead  are  partly  oxide, 
partly  salt ;  they  are  dyad,  while  the  second  atom  of  lead 
is  tetrad. 

It  is  possible  to  regard  nitric  peroxide  in  this  light 
as  a  nitrate  of  nitrosyl,  O=N— NO3  ;  but  its  easy  decom- 
position into  NO2  when  heated  militates  against  the 
view.  Compounds  of  antimony  and  bismuth,  having  the 


102  MODERN  CHEMISTRY 

formula*  Sfe-2O4  '.arid  Ei,jO44  inay  be  similarly  regarded 
as  O=Sb(SbO3)  and  G>=Bi(BiO3)  ;  of  this,  however, 
there  is  no  proof. 

Manganese  and  chromium  also  form  "  dioxides,"  to 
which  the  simple  formulas  MnO2  and  CrO9  are  usually 

o  '     ,o 

attributed  ;    they,   too,    may   be   written         x/Ci\         /Cr 

O^      XX 

o,    TI   xx 

and         VMn/        />Mn".     They   would   then   be   termed 

O^         NX 

chromous  chromate  and  manganous  manganate.  Such 
ideas  must  be  regarded  as  speculative,  but  there  can  be  little 
doubt  that  the  formulae  are  more  complex  than  they  are 
usually  written.  The  former  is  a  snuff-coloured  powder, 
produced  by  the  action  of  nitric  oxide  on  a  chromate  ;  the 
latter,  formed  by  oxidising  and  precipitating  a  manganous 
salt  simultaneously,  is  best  prepared  in  a  hydrated  state  by 
the  action  of  a  hypobromite  on  a  manganous  salt:  MnCl9.Aq 
4-NaOBr.Aq  +  2NaOH.Aq  -  O=Mn(OH)2  +  NaBr.Aq 
+  2NaCl.Aq.  It  is  a  common  black  mineral  in  the  anhy- 
drous state,  and  is  known  as  pyrolusite.  It  will  be  re- 
membered that  the  ordinary  method  of  preparing  chlorine  is 
to  heat  this  mineral  with  dilute  hydrochloric  acid,  and  also 
that  on  heating  alone  it  furnishes  oxygen,  being  itself  con- 
verted into  Mn3O4,  a  brown  powder,  which  may  be  formu- 
lated as  a  spinel,  viz.  (O=Mn— O)2=Mn. 

In  concluding  this  chapter  on  neutral  oxides,  it  may  be 
mentioned  that  there  are  a  few  which,  acting  generally  as 
feeble  bases,  yet  display  feebly  acid  properties  if  in  the 
presence  of  a  strong  base  like  soda  or  potash.  Such  are 
the  oxides  of  gold,  the  metals  of  the  platinum  group, 
and  of  titanium,  zirconium,  and  thorium.  The  chlorides 
of  these  elements  are  soluble  in  water,  as  also  the  sulphates 
and  nitrates  of  the  last  three.  Sulphates  of  gold  and  plati- 
num, however,  are  hydrolysed  by  water,  giving  oxides  and 
sulphuric  acid,  thus :  Pt(SO4)2  +  zHOH  =  PtO2  +  2H2SO4. 


NEUTRAL  OXIDES  103 

Salts  of  these  elements,  on  treatment  with  soda,  yield  no  pre- 
cipitate, for  they  are  dissolved  by  the  alkali ;  the  compounds 
formed  are  indefinite,  but  it  may  be  supposed  that  they 
contain  aurate,  MAuO2.Aq,  or  platinate,  titanate,  zirconate, 
or  thorate,  MPtO3.Aq,  &c.  Iron  and  calcium  titanates 
occur  native  ;  FeTiO3  is  termed  ilmenite,  and  CaTiO3 
perowskite.  The  first  is  isomorphous  with  and  crystal- 
lises along  with  native  ferric  oxide  ;  the  ore  is  known  as 
"  titanic  iron  ore."  It  is  the  commonest  compound  of 
titanium. 


CHAPTER  VI 

Anhydrides  —  Acids  and  Salts  — Basic  and  Acid 
Chlorides— The  Borates—The  Carbonates  and 
Thiocarbonates — Other  Acids  containing  Car- 
bon; their  Salts  with  Alcohol  Radicals— The 
Silicic  Acids  and  the  Silicates. 

Basic  Salts. — Many  compounds  are  known  which  are 
at  the  same  time  chloride  and  oxide,  or  chloride  and  hydr- 
oxide of  elements.  Where  the  element  with  which  the 
oxygen  and  chlorine  is  combined  is  one  which  forms  a  basic 
oxide,  the  compounds  in  question  are  termed  basic  chlorides. 
Similarly,  there  are  basic  bromides  and  iodides.  For  ex- 
ample, zinc  oxide  heated  with  zinc  chloride  forms  oxychlo- 
rides,  of  which  the  simplest  example  is  Cl~~Zn~~O~Zir~Cl; 
aluminium  chloride,  evaporated  with  water,  has  its  chlo- 
rine gradually  replaced  by  hydroxyl,  forming  successively 
C12=A1(OH),  C1-A1=(OH)2,  and  finally,  A1(OH)8, 
though  at  a  temperature  sufficient  to  complete  the  reaction, 
the  aluminium  would  probably  form  the  condensed  hydr- 
oxide O=A1OH  instead  of  the  trihydroxide.  We  shall 
see  later  that  other  groups,  playing  a  part  analogous  to 
that  of  the  chlorine  in  a  basic  salt,  may  also  exist  in  basic 
salts. 

Acid  Chlorides. — Another  class  of  double  oxides  and 
chlorides  exists,  most  of  which  are  easily  volatile,  and 
which  therefore  are  of  known  molecular  weight.  These 
are  the  so-called  "acid  chlorides" — oxychlorides  of  those 
elements  which  form  acids.  These  are  related  to  acids,  in 
as  much  as  by  replacement  of  their  chlorine  by  hydroxyl, 


BORATES  105 

acids  are  formed.  It  will  therefore  be  convenient  to  con- 
sider them  along  with  the  acids  to  which  they  are  related. 

A  general  idea  has  already  been  given  of  the  nature  of 
acids  in  describing  the  hydroxides  of  zinc  and  of  aluminium. 
As  a  rule,  acids  are  condensed  hydroxides  ;  that  is, 
hydroxides  which,  having  lost  the  elements  of  water,  are 
partly  oxides,  partly  hydroxides.  They  also  possess  the 
property  of  ionising  into  one  or  more  hydrogen  ions  and  an 
electro-negatively  charged  radical.  In  following  the  order 
of  the  periodic  table,  after  such  feebly  acidic  hydroxides  as 
those  of  zinc  and  aluminium,  hydroxide  of  boron  claims 
attention. 

Borates. — In  certain  lakes  in  California  the  water, 
when  evaporated,  deposits  crystals  of  the  formula 
Na2B4OrioH2O  ;  this  substance  is  named  borax.  It  is  a 
white,  crystalline  salt,  easily  soluble  in  hot  water, but  sparingly 
soluble  in  cold.  When  mixed  with  sulphuric  acid  nacreous 
scales  separate  of  the  formula  B(OH)3,  or,  as  it  is  usual  in 
writing  the  formulas  of  acids  to  place  the  hydrogen  atoms 
first,  H3BO3.  Boracic  acid  hardly  deserves  the  name  of 
acid  ;  in  aqueous  solution  it  exists  almost  entirely  in  the 
non-ionised  state.  No  ions  are  volatile  ;  but  this  compound 
issues  in  Tuscany  and  in  the  Lipari  Islands  along  with 
steam  from  cavities  in  the  ground,  termed  suffioni ;  it  is 
easily  recognised,  for  it  imparts  a  green  colour  to  a  flame 
held  in  the  steam.  When  heated  to  100°  boracic  acid  loses 
water  and  is  changed  into  metaboracic  acid,  O=B-OH, 
a  vitreous  substance ;  and  at  a  red-heat  boron  oxide, 
Bi;O3,  is  left  as  a  transparent,  colourless  glass.  Its  con- 
stitution is  O=B— O— B=O. 

The  borates  of  the  alkalies  are  prepared  by  mixing 
boracic  acid  with  the  hydroxide  of  the  alkali  metal ; 
although  there  are  very  few  hydrogen  ions  in  an  aqueous 
solution  of  boracic  acid,  however  dilute,  yet  some  of  those 
present  combine  with  the  hydroxyl  ions  of  the  alkali,  forming 

water,  thus:    H3BO3.Aq  +  3NaOH.Aq  =  Na3BO3.Aq  + 


io6  MODERN   CHEMISTRY 

3H2O.  But  there  are  so  few  ions  present,  that  those  of 
the  water,  which,  it  will  be  remembered,  is  ionised,  although 
to  an  extremely  minute  extent,  are  yet  sufficiently  numerous 
to  bear  some  proportion  to  those  of  the  boracic  acid  ;  hence 
the  reaction  given  above  is  perceptibly  reversed,  and  on 
dissolving  borax  in  water  it  is  "  hydrolysed,"  that  is,  split 
"by  the  hydrogen  and  hydroxyl  ions  of  the  water  into  non- 
ionised  boracic  acid  and  caustic  soda,  the  latter,  of  course, 
largely  ionised  as  usual.  It  is  therefore  possible  to  estimate 
the  sodium  of  borax  by  addition  of  a  solution  of  a  strong 
acid,  such  as  hydrochloric  or  sulphuric  acid  of  known  con- 
centration, just  as  if  no  boracic  acid  were  present,  provided 
methyl-orange  be  used  as  an  indicator.  (See  p.  75.) 
Thus  the  addition  of  36.5  grams  (H=i;  01  =  35.5) 
of  hydrochloric  acid,  dissolved  in  a  litre  of  water  (such  a 
solution  is  termed  a  "normal  solution"),  to  191  grams  of 
a  solution  of  crystallised  borax  in  a  litre  of  water  (1/2 
[Na2  =  46  +  B4  =  44  +  O7  =  112  +  ioH2O  =  180])  ;  (in 
all  1/2  of  382)  gives  a  solution  which  is  neutral  to  methyl- 
orange. 

Fused  borax  has  the  property  of  dissolving  oxides  of  the 
metals,  forming  complex  borates ;  certain  of  these  are 
coloured,  and  their  formation  is  often  made  use  of  for 
detecting  the  presence  of  such  metals  as  copper  (blue), 
silver  (yellow),  chromium  (green),  ferric  iron  (yellow), 
ferrous  iron  (bottle-green),  manganese  (amethyst,  when 
heated  in  a  flame  containing  excess  of  oxygen),  cobalt 
(blue),  and  nickel  (reddish).  Borax  is  also  used  for 
soldering  easily  oxidisable  metals,  such  as  iron,  copper,  or 
brass  ;  the  film  of  oxide  which  prevents  the  metal  touching 
and  alloying  with  the  solder  is  thus  removed.  Both  borax 
and  boracic  acid  have  considerable  antiseptic  properties,  and 
are  used  for  preserving  eggs,  milk,  and  other  animal  and 
vegetable  substances. 

Carbonates  and  Thiocarbonates.  —  The  car- 
bonates and  the  thio carbonates  are  derivatives  of  carbon 
dioxide  (or  '  rather  of  carbon  oxy-hydroxide,  commonly 


CARBONATES  107 

called  carbonic  acid),  and  of  carbon  disulphide.  Carbon  is  a 
tetrad,  and.  the  analogue  of  carbon  tetrachloride  would  be  the 
tetrahydroxide,  C(OH)4;  but  this  body  is  unstable,  and 
its  first  anhydride,  O=C(OH)2,  is  known  only  in  aqueous 
solution.  However,  carbonyl  chloride,  O=CC12,  exists  ; 
it  is  produced  by  the  direct  union  of  carbonic  oxide  with 
chlorine,  when  a  mixture  of  both  gases  is  exposed  to 
sunlight ;  it  was  formerly  known  as  "  phosgene  gas," 
meaning  "made  by  light";  but  it  is  more  conveniently 
prepared  by  passing  a  mixture  of  the  two  gases  over 
animal  charcoal  heated  to  redness.  It  condenses  to  a 
liquid,  boiling  at  8.4°.  It  is  immediately  decomposed  by 
water,  thus:  O=CC12  +  2HOH  =  O=C(OH)2+ 2HC1; 
if  sufficient  water  is  present,  the  carbonic  acid  can  remain 
in  solution.  The  existence  of  the  oxychloride  establishes 
the  formula  of  carbonic  acid. 

Carbonic  acid  is  a  very  easily  decomposable  substance ; 
if  liberated,  unless  a  great  deal  of  water  be  present,  it  splits 
into  its  anhydride,  CO2,  and  water:  O=C(OH)2  =  CO0 
+  H2O.  The  anhydride  is  a  colourless  gas,  which  con- 
denses to  a  solid  at  about  —80°  ;  it  can  be  liquefied  only 
under  pressure.  Carbon  dioxide,  or  carbonic  anhydride, 
is  produced  by  heating  a  carbonate  ;  as  already  remarked, 
all  carbonates,  except  those  of  the  alkaline  metals,  are 
decomposed  by  heat,  forming  oxides,  and  evolving  carbon 
dioxide.  It  is  also  produced  when  carbon  or  carbon 
monoxide  is  burned  with  excess  of  oxygen.  Lastly,  it  is 
produced  in  large  quantities  during  the  process  of  fermenta- 
tion. Glucose,  or  grape  sugar,  either  produced  by  the 
hydrolysis  of  starch  or  extracted  from  fruits  like  grapes, 
when  mixed  in  dilute  aqueous  solution  with  yeast,  a  vegetable 
organism,  decomposes  into  ethyl  alcohol  and  carbon  dioxide, 
thus:  C6H12O6  =  2C2H5OH  +  2CO2.  The  carbon  di- 
oxide being  heavier  than  air,  collects  in  the  fermenting 
tuns  ;  it  is  now  often  collected  and  compressed  until  it 
liquefies  ;  and  the  liquid  on  expansion  solidifies  to  a  snow- 
like  solid,  used  for  producing  low  temperatures. 


io8  MODERN   CHEMISTRY 

A  solution  of  carbonic  anhydride  in  water  contains 
carbonic  acid,  O=C(OH)9,  which  is  a  very  weak  acid 
owing  to  the  small  extent  of  its  ionisation.  It  is  probable, 
too,  that  liquid  carbon  dioxide  exists  in  the  solution,  mixed, 
but  not  combined  with  the  water.  Carbonic  acid  reacts 
with  sodium,  potassium,  calcium,  or  barium  hydroxide, 

f    -  -  +   • 

forming  carbonate  of  the  metal:  H2CO3.Aq  +  zNaOH.Aq 

=  Nt2C03.Aq  +  2H20  ;  H2C03.Aq  +  Ca(OH)2.Aq - 
CaCO3  +  2H9O.  In  such  actions  it  is  only  the  ionised 
portion  of  the  acid  which  reacts,  and  the  hydrogen  ions 
form  water  ;  when  these  are  removed  another  portion 
becomes  ionised  in  order  to  restore  equilibrium  ;  it  reacts  in 
its  turn  until  all  has  become  transformed.  On  evaporation 
of  the  solution  the  alkaline  carbonate  is  left  as  a  white  crystal- 
line salt;  hydrated  sodium  carbonate,  Na9CO3.  ioH2O, 
is  ordinary  washing-soda.  All  other  carbonates  are  insol- 
uble in  water,  and  are  consequently  thrown  down  as 
precipitates  on  adding  a  solution  of  sodium  carbonate  to 
any  ionised  solution  of  other  metals.  They  form  flocculent 
precipitates,  generally  possessing  the  colour  of  the  ion 
of  the  metal ;  thus  copper  carbonate  is  blue,  ferrous 
green,  cobalt  pink,  and  so  on.  But  with  the  exception  of 
the  carbonates  of  the  metals  of  the  sodium  and  calcium 
groups  all  other  precipitated  carbonates  are  "  basic,"  that 
is,  they  are  partly  hydroxides,  partly  carbonates.  Copper 
carbonate,  for  example,  may  be  assigned  the  formula 

/O-Cu-OH 
O=C<f  ;    it  will   be  noticed  that  each  atom 

X0-Cu-OH 

of  copper  is  combined  with  the  oxygen  of  the  carbonic 
residue  on  the  one  hand,  and  with  hydroxyl  on  the  other. 
The  paint  known  as  "  white  lead "  consists  of  a  basic 
carbonate  of  lead,  more  complex  than  the  example  given 
above,  of  the  formula 

HO-Pb-0-(CO)-0-Pb-0-(CO)-0-Pb-OH. 

Native  Carbonates. — Many  carbonates  exist  in  the 


ACID  CARBONATES  109 

native  state  ;  some  are  widely  distributed  minerals.  Among 
these  are  Iceland  or  calc-spar,  arragonite,  limestone, 
chalk,  and  marble,  all  of  them  calcium  carbonate; 
strontianite,  SrCO3 ;  witherite,  BaCO3 ;  spathic  iron 
ore,  FeCOs,  also  named  clay-band  when  contaminated 
with  clay,  and  black-band  when  mixed  with  shale. 
Magnesite  is  MgCO3  ;  dolomite,  a  mixture  of  magne- 
sium and  calcium  carbonates ;  calamine,  ZnCO3 ;  and 
cerussite,  PbCO3.  Malachite  and  azurite  are  basic  car- 

/O-Cu-OH 
bonates  of  copper,  O=C\  ,  and 

X0-Cu-OH 
O  O 

HO-Cu-0-C-O-Cu-O-C-O-Cu-OH. 

We  see  here  again  that  with  weak  bases,  such  as  the 
hydroxides  of  most  metals,  the  carbonates  tend  to  become 
basic,  that  is,  to  be  hydrolysed.  This  is  why  the  preci- 
pitates obtained  on  adding  a  soluble  carbonate  to  a  salt  of 
such  metals  are  basic,  and  not  normal  carbonates. 

"Acid"  Carbonates. — The  name  "acid  carbon- 
ate "  is  given  to  a  double  carbonate  of  hydrogen  and  a 
metal.  Such  bodies  are  prepared  by  the  method  which 
always  is  adopted  for  the  preparation  of  double  salts — by 

/ONa 
mixture.     Hydrogen  sodium  carbonate,  O=C\          ; 

XOH 

the  corresponding  potassium  compound  ;  hydrogen  cal- 
O  O 

I!  II 

cium  carbonate  HO-C-  O-Ca-O-C-OH,  a  ferrous 
carbonate  of  similar  formula,  and  many  others  are  all 
formed  when  carbonic  acid  and  the  respective  normal  car- 
bonate are  mixed,  the  mixture  being  kept  cold.  On  raising 
the  temperature  of  all  of  these,  carbon  dioxide  escapes,  and 
the  neutral  carbonate  is  again  formed.  "  Acid  "  carbonate 
of  sodium  is  the  common  "  baking-soda  ;  "  hydrogen  calcium 


no  MODERN   CHEMISTRY 

carbonate  is  a  constituent  of  many  natural  waters,  and  is  the 
cause  of  what  is  termed  "  temporary  hardness  "  ;  for  on 
boiling  the  water  the  neutral  carbonate  is  precipitated,  and 
the  water  ceases  to  be  "hard."  The  same  result  may  be 
effected,  paradoxical  as  it  may  appear,  by  the  addition  of 
lime-water  ;  for  then  sufficient  calcium  hydroxide  is  present 
to  form  normal  calcium  carbonate  with  the  hydrogen  carbon- 
ate, thus :  Ca(HCO3)2.Aq  +  Ca(OH)2.Aq  =  2CaCO3  + 
2H2O.Aq.  Hydrogen  ferrous  carbonate  is  a  constituent 
of  chalybeate  springs  ;  on  exposure  to  the  atmosphere  the 
iron  is  oxidised  to  ferric  hydroxide,  and  the  carbonic  acid, 
being  too  weak  an  acid  to  form  a  carbonate  with  such  a 
weak  base  as  that,  escapes:  2Fe(HCO3)2.Aq+  5H2O  + 
O  =  2Fe(OH)3  +  4H2CO3.Aq.  The  ferric  hydroxide  is 
deposited  as  a  brown  scum  on  the  banks  of  the  streams 
flowing  from  such  wells. 

Carbonates  of  Radicals. — Although  normal  hydr- 
oxide of  carbon  is  unknown,  yet  if  the  hydrogen  be  replaced 
by  ethyl,  — C2H5,  the  compound  is  stable.  The  compound, 
which  is  produced  by  the  action  of  carbon  tetrachloride 
on  sodium  ethoxide,  CC14  +  4Na-O-Ck>H5  =  4NaCl  + 
C(O-C2H5)4,  is  the  analogue  of  C(OH)4.  It  is  a 
volatile  liquid,  and  is  named  ethyl  orthocarbonate.  And 
a  corresponding  carbonate  of  ethyl,  O=C(OC2H5)2,  the 
analogue  of  carbonic  acid,  O=C(OH)2,  is  formed  by  treating 
carbonyl  chloride 'with  alcohol:  O=CCU  +  2HO-C2H5= 
O=C(OC2H5)2  +  2HC1.  These  compounds  are  volatile, 
and  can  be  weighed  in  the  state  of  vapour,  hence  their 
molecular  weights  are  known,  and  this  is  an  additional 
proof  of  the  correctness  of  the  formulae  ascribed  to  carbonic 
acid  and  the  carbonates. 

Thiocarbonates. — The  sulphocarbonates,  or  thiocar- 
bonates  (from  the  Greek  theion,  sulphur)  form  a  class 
of  salts  analogous  to  the  carbonates,  both  in  their  formulas 
and  in  the  method  of  their  preparation.  Carbon  disulphide, 
a  volatile  liquid,  boiling  at  46°,  possessing  a  disagreeable 
smell,  is  produced  when  sulphur  vapour  is  led  over  charcoal 


THIOCARBONATES  in 

heated  to  redness  in  a  fireclay  tube  ;  in  fact,  the  carbon  is 
burned  in  sulphur  gas.  When  shaken  with  a  concentrated 
aqueous  solution  of  the  sulphide  of  sodium  or  potassium,  it 
dissolves,  forming  the  compound  Na2CS3,  or  K9CS3. 
These  thiocarbonates,  like  the  carbonates,  are  white,  crystal- 
line salts  ;  on  adding  acid,  thiocarbonic  acid  separates  as 
an  oil ;  it  slowly  decomposes,  especially  if  warmed,  into 
hydrogen  sulphide  and  carbon  disulphide.  Many  of  its  salts 
are  insoluble,  and  may  be  prepared  by  precipitation. 

The  formula  of  carbon  dioxide  is  CO2,  that  of  carbon 
disulphide  CS2  ;  and  it  is  evident  that  an  intermediate 
substance  should  exist  of  the  formula  COS.  This  sub- 
stance is  carbon  oxysulphide.  It  is  a  gas,  prepared  by 
heating  thiocyanic  acid,  HSCN,  the  ammonium  salt  of 
which  is  produced  when  ammonia  is  passed  through  a 
mixture  of  carbon  disulphide  and  alcohol :  CS2  +  2NH3.Alc 
=  H2S  +  (NHJSCN.Alc.  On  evaporation  of  the  alcohol 
the  ammonium  thiocyanate  crystallises  out.  This  salt,  dis- 
tilled with  sulphuric  acid,  yields  in  passing  the  acid  HSCN, 
which,  on  account  of  the  high  temperature,  reacts  with 
water,  forming  ammonia  (which  yields  ammonium  sulphate 
with  the  sulphuric  acid)  and  carbon  oxysulphide,  COS  : 
HSCN  +  H2O  -  NH3  +  COS. 

Like  nitrous  oxide,  carbon  disulphide  is  an  endothermic 
compound,  and  can  consequently  be  decomposed  by  shock  ; 
when  a  fulminate  is  exploded  in  it,  it  is  resolved  into  carbon 
and  sulphur.  On  the  other  hand,  carbon  dioxide  and  oxy- 
sulphide are  exothermic  compounds,  heat  being  evolved 
during  their  formation. 

Acids  containing  Carbon. — An  enormous  number 
of  acids  containing  carbon  is  known,  in  which  the  acidic 
carbon  atom  is  combined  with  oxygen  and  hydroxyl,  and 
also  with  hydrocarbon  residues,  such  as  methyl  or  ethyl,  or  with 
some  more  complex  group  of  carbon  atoms.  The  simplest 

O 

of   these    is    formic    acid,    H— C— OH.      Acetic    acid    is 


ii2  MODERN   CHEMISTRY 

O 

II 

methyl-formic  acid  (CH3)— C— OH  ;  ethyl-formic  acid  is 

O 
ll 
named  propionic  acid  ;  its  formula  is  CH3— CH2— C— OH. 

0=>C-OH 
Oxalic  acid  is  to  be  regarded  as  di-carboxyl,          I  , 

O=C-OH 

the  name  carboxyl  being  a  contracted  form  of"  carb(onyl 
hydr)oxyl"  ;  it  is  commonly  written  —CO— OH. 

Formic  acid  (from  formica,  an  ant)  is  contained  in  ants 
and  stinging  nettles.  Sodium  formate  is  produced  when 
carbon  monoxide  is  left  in  contact  with  sodium  hydroxide  ; 
the  reaction  takes  a  considerable  time:  CO+NaOH  = 
H— CO— ONa.  It  is  also  formed  by  heating  oxalic  acid, 
better  in  presence  of  glycerine:  (CO— OH)2  =  CO0  + 
H— CO— OH.  It  is  a  colourless,  pungently  smelling  liquid, 
boiling  at  99°,  and  a  fairly  strong  acid  in  aqueous  solution  ; 
it  is  poisonous.  Its  salts  are  crystalline,  and  possess  the 
colours  of  the  metallic  ions  which  they  contain.  When 
warmed  with  concentrated  sulphuric  acid,  or  with  other 
substances  capable  of  withdrawing  water,  it  yields  carbon 
monoxide.  Yet  CO  is  not  the  true  anhydride  of  formic 
acid,  seeing  that  an  anhydride  can  be  obtained  only  from 
loss  of  the  elements  of  water  from  hydroxyl  groups,  for 
formic  acid  contains  the  group  H— C=  ;  the  real  anhydride 

o      o 

would  be  H— C— O— C— H  ;  it  is  unknown. 

Acetic  acid  is  the  acid  constituent  of  vinegar,  and  is  a 
solid,  melting  at  17°  to  a  liquid,  boiling  at  118°.  It  can 
be  formed  synthetically  by  bringing  into  contact  carbon 
dioxide  and  sodium  methide,  a  compound  of  the  formula 
Na-CH3  ;  the  equation  is  :  Na-CH3  +  CO2  = 
H3C— CO— ONa  ;  the  sodium  salt,  distilled  with  sulphuric 
acid,  yields  acetic  acid.  It  is  produced  on  a  large  scale  by 
the  distillation  of  wood  ;  the  distillate  consists  mainly  of 


"ORGANIC  ACIDS"  113 

acetic  acid  and  methyl  alcohol  ;  it  is  neutralised  with  lime, 
and  distilled,  when  the  alcohol  passes  over,  leaving  behind 
the  calcium  acetate  ;  this  is  evaporated  to  dryness,  and 
heated,  so  as  to  char  tarry  matters,  also  produced  when 
wood  is  distilled  ;  the  calcium  salt  is  finally  distilled  with 
sulphuric  acid.  Acetic  acid  is  also  formed  by  the 
oxidation  of  aldehyde  (p.  88),  which  is  itself  an  oxi- 
dation-product of  alcohol.  The  connection  between 
these  bodies  is  :  CH3-CH2-OH,  CH3-CH=O,  and 
O 
ii 

CH3— C— OH.  Aldehyde  may  be  regarded  as  the 
anhydride  of  CHg— CH=(OH)2,  and  acetic  acid  of 
CH3  =  C(OH)3.  The  usual  oxidising  agent  is  chromic 
acid  ;  if  the  product  of  oxidation  is  conveyed  away  as  it  is 
formed  by  sloping  the  condenser  downwards,  aldehyde  is 
obtained  ;  if  the  aldehyde  is  returned  to  the  oxidising 
mixture  by  sloping  the  condenser  upwards,  and  cooling  with 
ice  and  water,  the  product  is  acetic  acid.  The  oxidation  is 
also  effected  by  an  organism  called  "  mother  of  vinegar  "  ; 
sour  wine  or  beer  is  allowed  to  trickle  down  a  cask  filled 
with  shavings  of  beech-wood,  on  which  the  slimy  masses 
of  the  organism  are  growing  ;  oxygen  enters,  and  the  vinegar 
flows  out  at  the  bottom  of  the  cask. 

On  distilling  acetic  acid  with  phosphorus  pentachloride, 
hydroxyl  is  exchanged  for  chlorine  :  4CH3— CO— OH  + 
PC15  =  4CH3-CO-C1  +  H8PO4  +  HC1.  the  compound 
obtained  is  named  acetyl  chloride  ;  acetic  acid  may  be 
regarded  as  hydroxide  of  the  group  (CHg— C=O)— ,  and 
on  treating  acetyl  chloride  with  water  it  is  at  once  formed  : 
CH3-COC1  +  H-OH  =  CH3-CO-OH  +  HC1. 
And  aldehyde  may  be  regarded  as  a  hydride  of  acetyl, 
(CH3— CO)— H.  A  similar  body  cannot  be  made 
from  formic  acid,  for  it  decomposes  into  carbon  monoxide 
and  hydrogen  chloride  :  H-CO-C1  =  CO  +  HC1. 

Oxalic  acid  is  contained  as  hydrogen-potassium  salt  in 
the  plants  sorrel  and  rumex.  It  can  be  prepared  by  the 


ii4  MODERN   CHEMISTRY 

oxidation  of  sugar  with  concentrated  nitric  acid,  or  by 
heating  sawdust  with  a  mixture  of  caustic  soda  and  potash 
in  shallow  trays ;  on  treating  the  charred  residue  with 
water,  sodium  oxalate,  a  comparatively  insoluble  salt,  remains, 
while  the  excess  of  alkali  dissolves  ;  the  sodium  oxalate 
is  extracted  with  boiling  water,  and  calcium  chloride  is 
added  ;  this  precipitates  the  almost  insoluble  calcium 
oxalate ;  and  on  digesting  it  with  the  equivalent  amount 
of  sulphuric  acid,  sparingly  soluble  calcium  sulphate  remains, 
while  oxalic  acid  dissolves.  The  filtered  solution,  when 

C(OH)3 
evaporated,  deposits  crystals  of  ortho-oxalic  acid,  | 

C(OH)3 
CO-OH 
which,  at   100°,  dehydrate  to    I  .       Oxalic  acid  is 

CO-OH 

a  di-basic  acid,  and  its  salts,  like  those  of  formic  and  acetic 
acids,  have  the  colour  of  the  positive  ion.  It  cannot  be 
dehydrated  further,  for  the  anhydride,  which  should  possess 

CO 
the  formula  P>O,  decomposes  into  CO  and  CO2. 

CO 

Salts  of  these  acids  with  alcohol  radicals,  such  as 
methyl  and  ethyl,  are  prepared  by  saturating  a  solution  of 
the  acid  in  the  respective  alcohol  with  hydrogen  chloride, 
and  then  distilling:  (COOH)2  +  2CH3OH  =  (COOCH3)9 
+  2HOH.  The  hydrogen  chloride  serves  to  withdraw 
water,  and  prevent  it  acting  on  the  product.  Such  salts5 
which  are  generally  colourless  liquids  or  solids,  possessing 
a  pleasant  smell,  are  called  "  esters.7'  As  a  rule  they  are 
sparingly  soluble  in  water,  and  are  not  ionised  in  solution, 
thus  differing  from  salts  of  the  metals.  When  boiled  with 
alkalies,  the  ester  being  returned  by  means  of  an  inverted 
condenser  into  the  boiling-flask,  they  change  into  salts  of  the 
alkalies,  and  the  alcohol:  CH0-CO-O-CH2-CH3  + 
KOH.Aq  ---.  CH3-CO-OK.Aq  +  CH3-CHL-OH. 
This  change  is  also  effected  by  heating  with  water  in  a 


SILICIC  ACIDS  115 

sealed  tube ;  it  is  accelerated  by  the  presence  of  hydrogen 
ions,  and  therefore  by  the  presence  of  strong  acids,  such  as 
hydrochloric  acid.  Decomposition  of  this  kind  by  alkalies 
is  called  "  saponification  "  ;  if  effected  by  water  the  term 
"  hydrolysis  "  is  applied  to  it. 

Silicic  Acids  and  Silicates. — While  the  character- 
istic of  carbon  is  to  form  compounds  in  which  many  atoms 
of  carbon  are  linked  together  (hydrocarbons,  for  example, 

H    H    H  H    H 

having  formulse  like  H-C-C-C-  ...  -C-C-H), 

H    H    H  H    H 

atoms  of  silicon  are  characterised  by  linking  by  means  of 
atoms  of  oxygen.  This  peculiarity  leads  to  the  existence 
of  a  large  number  of  silicates,  and  probably,  too,  of  a 
large  number  of  silicic  acids.  The  existence  of  some  of 
these  is  rendered  certain  by  a  study  of  the  oxychlorides. 

Silicon  tetrachloride,  SiCl4,  when  passed  over  fragments 
of  felspar  (a  silicate  of  aluminium  and  calcium)  heated  to 
whiteness  in  a  porcelain  tube,  exchanges  chlorine  for  oxygen, 
and  yields  a  liquid  boiling  at  about  137°,  of  the  formula 

/SiCl, 

O<Q  .     This  liquid,  passed  along  with  oxygen  through 

\SiCl, 

a  hot  glass  tube,  gave  two  other  liquids,  which  could  be 
separated  by  fractionation ;  the  one,  boiling  at  153°,  had 
the  formula  Si4(XCl10,  and  the  other,  boiling  at  200°, 
Si4O4Clg.  The  vapour-densities  of  these  liquids  were 
determined,  and  led  to  the  formulae  given  above.  The 
signification  of  this  will  appear  presently. 

Si(OH)4.  When  silica,  in  the  form  of  flint,  or  fine 
sand,  or  powdered  rock-crystal  is  either  fused  with  caustic 
soda  or  potash,  or  heated  under  pressure  with  a  solution 
of  one  or  other  of  the  alkalies,  an  orthosilicate  is  pro- 
duced, possessing  the  formula  Si(ONa)4  or  Si(OK)4. 
These  silicates  are  soluble  in  water,  and  as  they  resemble 
glass  in  appearance,  they  are  usually  named  "  soluble  glass." 
If  hydrochloric  acid  is  added  to  the  solution  of  one  of 


ii6  MODERN  CHEMISTRY 

them,  no  apparent  change  occurs ;  in  reality,  orthosilicic 
acid  is  produced,  a  compound  which  is  hardly  ionised  at 
all,  being  one  of  the  very  weakest  of  acids. 

Osmosis. — To  separate  the  ions  of  sodium  chloride 
and  of  hydrochloric  acid  advantage  is  taken  of  a  discovery 
made  by  Graham,  that  a  vegetable  or  animal  membrane  like 
parchment  or  parchmentised  paper  is  readily  permeated  by 
crystalline  bodies,  while  it  is  very  slowly  permeated  by 
"  colloidal "  or  gum-like  compounds.  By  placing  in  a 
drum,  floating  on  water,  the  mixture  of  orthosilicic  acid 
and  salt,  the  sodium  and  chlorine  ions  pass  through,  of 
course  in  equivalent  proportions,  leaving  the  colloid  behind. 
Fresh  water  is  substituted  from  time  to  time,  until  all 
chlorine  ions  have  been  removed  from  the  silicic  acid.  The 
water  can  be  removed  by  evaporation  in  vacua,  and  a  clear 
but  very  viscous  liquid  remains,  which  is  believed  to  con- 
tain Si(OH)4.Aq.  On  raising  the  temperature  of  this 
viscous  liquid  it  gelatinises,  and  is  then  insoluble  in  water ; 
the  resulting  compound  may  have  a  formula  analogous  to 
carbonic  acid,  O=Si(OH)2;  it  is  termed  metasilicic 
acid.  On  further  drying,  water  is  gradually  expelled,  and 
finally  a  flint-like  mass  is  left,  which  on  ignition  yields 
a  white  powder  of  SiO2,  or  silica.  As  already  mentioned, 
silica  is  found  in  nature ;  when  pure,  it  crystallises  in 
hexagonal  prisms,  and  is  termed  quartz,  rock-crystal,  or 
Irish  diamond.  It  is  used  for  spectacle  lenses  and  optical 
instruments. 

The  major  part  of  the  rocks  which  constitute  the 
surface  of  the  earth  consists  of  mixtures  of  silicates. 
Occasionally  they  are  found  in  definite  crystals,  and  on 
analysis  their  formulae  can  be  determined.  From  their 
formulas,  the  formulas  of  the  silicic  acids  from  which 
they  may  be  supposed  to  be  derived  can  be  deduced ; 
and  tables  follow,  in  which  the  formulas  of  these  silicic 
acids  and  of  some  of  the  minerals  constituting  their  salts 
are  given. 


SILICATES 


117 


OH 
OH 
OH 


Si 


O 
O 
0\ 


Be 


>Be 


Beryl. 


Al-Si04-Al 


Xenolite. 


Orthosflicates.  —  These  are  orthosilicates  ;  the 
comma  between  the  Mg  and  the  Fe  means  that  these 
metals  can  replace  each  other  in  any  proportions.  Xenolite, 
it  will  be  observed,  is  the  silicate  of  a  triad  metal,  aluminium  ; 
and  four  atoms  of  aluminium  replace  twelve  molecules  of 
hydrogen  in  three  molecules  of  orthosilicic  acid.  But 
double  silicates  are  common,  in  which  three  of  the  atoms  of 
hydrogen  in  three  molecules  of  orthosilicic  acid  may  be 
replaced  by  three  monad  atoms  ;  or  by  one  dyad  and  one 
monad  atom  ;  or  we  may  have  a  monad  group,  such  as 
-A1=O,  or  —  A1F2,  replacing  each  atom  of  hydrogen  ; 
or,  lastly,  the  aluminium  may  be  partly  hydroxide,  thus 
constituting  a  basic  silicate.  Examples  of  such  compounds 


Al-SiO4-Al 


Muscovite,  or  Potash  mica. 


Al-SiO4__CaH 


Prehnite. 


ii8  MODERN   CHEMISTRY 

Si04-(Al  =  0)3  Si04^(AlF2)3 

Al—  SiO4~Al  Al—SiCX-Al 


SiO4-Al 


Fibrolite.  Topaz. 

OH 


SiO4_Al 
Kaolin  or  China-clay. 

In  such  silicates,  the  aluminium  is  often  partially  replaced 
by  triad  metals,  such  as  triad  chromium,  iron,  or  man- 
ganese. 

Metasilicates.  —  Metasilicates  are  derivatives  of  the 
acid  H2SiO3  ;  the  constitutional  formula  is  O=Si(OH)2, 
like  that  of  carbonic  acid.  Examples  of  metasilicates 
are  :  — 


O=Si  Ca         O  =  Si  (Mg,  Fe",  Mn",  Ca) 

\0/  \0/ 

Wollastonite.  Augite  or  Hornblende. 

O  ° 

/    \  il 

O  =  Si  Al  -  O  -  Si  -  ONa 


Jade. 
The  potassium  salt  is  Leucite. 

Disilicates. — The  molecules  of  orthosilicic  acid  may 
lose  one  molecule  of  water,  the  remaining  atom  of  oxygen 
of  the  two  hydroxl  groups  serving  to  unite  the  two  molecules 


SILICATES 


119 


together,  and  a  similar  loss  of  water  may  be  repeated  twice, 
thus  : — 


orthosilicic  acid. 


OH 


NOH 

2nd  anhydride. 


Si(X 


Si00 


Silica. 


The  final  loss  of  water  yields  anhydrous  silica.  These 
acids  are  not  known  as  such  ;  but  certain  minerals  may  be 
regarded  as  their  salts.  It  is  probable  that  okenite  is  a 
disilicate,  thus  CaH4Si2O7  ;  and  also  petalite,  a  derivative 
of  its  second  anhydride,  AlLi(Si9O5)2.  Similarly,  three 
molecules  of  orthosilicic  acid,  by  losing  two  molecules  of 
water,  may  unite  to  form  trisilicic  acid  ;  and  it  again  by 
successive  loss  of  one,  two,  and  three  molecules  of  water 
may  yield  a  first,  a  second,  and  a  third  anhydride.  The 


120  MODERN   CHEMISTRY 

well-known  felspars  albite  and  orthoclase  are  salts  of  the 
third  anhydride  of  trisilicic  acid,  thus  : — 

XX  O  O 

/  \  II          II 

Al— O     Si  -O-Si-O-Si-  ONa 

N^ 

Albite. 

7o.  o         o 

/  \  II          II 

Al  -O— Si  -  O  -  Si  -  O  -  Si  -  OK 

\r 

Orthoclase. 

The  method  of  ascertaining  the  formula  of  a  silicate 
requires  notice.  In  order  to  determine  the  relative  number 
of  molecules  of  silica,  SiO2,  and  of  the  oxides  of  the  various 
metals  in  combination  with  it,  each  percentage  is  divided 
by  the  molecular  weight  of  the  oxide  in  question ;  the 
quotients  are  then  divided  by  the  smallest,  and  the  ratio 
between  the  resulting  quotients  compared.  To  take  an 
instance  : — 

An  analysis  of  a  specimen  of  muscovite  gave  the  toilow- 
ing  numbers  : — 

SiO2  =  45.07  per  cent.;  A12O8  =  38.41  ;  K2O  =  12.10; 
H9O  =  4.42;  together  =  i  oo.oo.  Dividing  by  60.4; 
by  102.3  ;  by  94.3  ;  by  18.0,  the  quotients  0.746,  0.375, 
0.128,  0.245  are  obtained.  Again  dividing  the  quotients 
by  0.128,  the  smallest  of  these  quotients,  the  ratios  are  : 
6,  3,  i,  2,  nearly.  Therefore  the  formula  is  6SiO9, 
3A12O3,  K2O,  2H2O,  or,  adding  the  various  constituents 
together  and  dividing  by  2,  Si3O10Al3KH2.  The  group 
Si3O10  is  3  x  SiO4 ;  the  compound  is,  therefore,  an  ortho- 
silicate  ;  and  three  atoms  of  triad  aluminium,  one  of  monad 
potassium,  and  two  of  monad  hydrogen  are  equivalent  to 
the  twelve  atoms  of  hydrogen  of  the  three  molecules  of 
orthosilicic  acid.  It  sometimes  happens,  however,  that  one 


SILICATES  121 

metal,  such  as  magnesium,  may  replace  more  or  less  of 
another,  such  as  calcium  and  iron.  In  that  case,  the 
quotients  obtained  on  dividing  the  percentages  by  the  mole- 
cular weights  are  added  before  the  final  ratio  is  obtained. 
The  products  of  Nature's  laboratory  are  seldom,  if  ever, 
pure  ;  and  it  rarely  happens  that  a  natural  mineral  gives 
results  so  easily  interpreted  as  the  case  given  above.  For 
the  mineral  no  doubt  separates  from  a  matrix  in  which 
many  compounds  are  present ;  and  so  it  happens  that  one 
metal  may  take  the  place  of  another  posses-sing  the  same 
valency,  and  capable  of  forming  compounds  of  the  same 
crystalline  form.  The  alkali  metals  are  mutually  replace- 
able ;  also  the  triads  Al,  Fe,  Mn,  Cr,  and  others.  There 
are  even  instances  where  silicon  is  partially  replaced  by 
titanium  ;  hence  the  interpretation  of  the  results  of  analyses 
presents  a  problem  of  no  small  difficulty.  The  work  of 
F.  W.  Clarke,  of  the  U.S.  Geological  Survey,  has  con- 
tributed not  a  little  to  a  solution  of  this  problem. 


CHAPTER   VII 

ANHYDRIDES,    ACIDS,    AND    SALTS 

Phosphoric,  Vanadic,  Arsenic,  and  Antimonic  Acids 
— Nitrous,  Phosphorous,  Arsenious  Acids — Phos* 
phatic  Acid — Hyponitrous  and  Hypophosphorous 
Acids,  and  their  Salts. 

THE  remaining  hydroxides,  which  all  exhibit  well-marked 
acid  functions,  may  be  divided  into  two  classes,  those  of 
elements  of  odd  valency,  and  those  derived  from  elements 
of  even  valency.  A  scheme  has  already  been  given  on 
p.  71,  which  illustrates  the  derivation  of  the  acids  of  the 
halogens  from  the  imaginary  hydroxides  corresponding  to 
Xvn,  Xv,  X111,  and  X1,  where  X  stands  for  halogen,  and 
the  Roman  numerals  for  the  valencies  in  the  compounds. 

Elements  of  Odd  Valency. — The  highest  valency 
shown  by  elements  of  the  nitrogen  group,  apart  from  a 
somewhat  questionable  pernitric  acid,  is  five.  This  is 
illustrated  by  the  formulx  of  the  pentoxides,  N0O5,  P9O5, 
As2O5,  Sb2O5,  and  V2O5.  But  these  compounds  possess 
very  different  stability,  and  the  elements  show  different 
behaviour  in  uniting  with  oxygen.  Nitrogen  and  oxygen 
do  not  unite  except  when  electric  sparks  are  passed  through 
a  mixture  of  the  two  gases,  or  when  a  high-tension  current 
is  passed  through  air.  It  is  doubtful  whether  heat  alone 
is  the  cause  of  this  union  ;  it  is  more  probable  that  energy 
must  be  imparted  to  the  combining  gases  in  an  electrical 
form.  The  act  of  combination,  in  which  the  product  is 
the  peroxide  NO2,  is  attended  by  absorption  of  heat  (7700 


PHOSPHORIC  ACIDS  123 

calories  for  the  union  of  14  grams  of  nitrogen  with  32  grams 
of  oxygen)  ;  and  this  energy  must  be  supplied  if  union  is 
to  take  place.  On  the  other  hand,  phosphorus  burns 
brilliantly  in  air,  and  if  excess  of  oxygen  be  present,  the 
so-called  pentoxide  is  produced  ;  according  to  the  vapour- 
density,  however,  the  formula  is  P4O10.  If  air  be  slowly 
passed  over  heated  phosphorus,  on  the  other  hand,  the 
lower  oxides  P4O6  and  P0O4  are  formed.  It  is  not  pos- 
sible to  dehydrate  phosphoric  acid,  HPO3,  completely,  so 
as  to  obtain  P0O5.  When  arsenic  burns  in  air,  arsenious 
oxide,  As4Ofi,  is  the  product ;  with  antimony,  Sb4O6  ;  but 
vanadium  pentoxide,  V2O5,  is  formed  when  the  element 
or  one  of  the  lower  oxides  is  heated  in  air. 

The  pentoxides  behave  differently  when  treated  with 
water.  While  N2O5  and  P4O10  unite  with  water  with  a 
hissing  noise  to  form  HNO3  and  HPO3,  As4O10  slowly 
reacts  to  produce  H3AsO4,  and  probably  H3VO4  is  the 
result  of  dissolving  V0O5  in  water ;  the  corresponding 
Sb9O5  is  insoluble  in  water. 

Acid  Chlorides. — The  clue  to  the  constitution  of  the 
acids  of  these  elements  is  aiforded  by  the  oxychlorides,  as 
in  the  case  of  carbon  and  silicon.  No  oxychloride  con- 
taining pentad  nitrogen  is  known,  but  phosphoryl  chloride, 
O=PC13,  and  antimonyl  chloride,  O=SbCl3,  are  pro- 
duced by  the  action  of  a  small  quantity  of  water  on  the 
respective  pentachlorides  :  C12=PC13  +  H2O  -  O=PC13  + 
2HC1.  The  former  is  a  colourless  liquid  boiling  at  107°, 
and  the  latter  a  white,  crystalline  solid.  Phosphoryl 
chloride  reacts  with  hydrogen  sulphide,  yielding  the  corre- 
sponding phosphoryl  sulphide :  O=PC13  +  H2S  -  S=PC13 
4-  H2O,  and  hydrogen  sulphide  acts  on  antimony  pen- 
tachloride,  with  formation  of  S=SbCl3.  O=VC13  is 
produced  by  direct  union  of  VO  with  chlorine.  It  is  a 
yellow  liquid  boiling  at  137°.  The  vapour-densities  of 
phosphoryl  and  vanadyl  chlorides  lead  to  the  ascribed 
formulas. 

Ortho~,  Pyro=,  and  Meta-Acids. — With   water, 


i24  MODERN   CHEMISTRY 

these  substances  exchange  chlorine  for  hydroxyl,  thus  : 
O=PC13  +  3H-OH  -  O=P(OH)3  +  sHCl.  This 
establishes  the  formula  of  ortho-phosphoric  acid.  The 
name  ought,  in  strictness,  to  be  applied  to  P(OH)5;  but, 
as  the  true  ortho-phosphoric  acid  is  unknown,  it  has  been 
transferred  to  what  should  be  termed  its  first  anhydride. 
The  corresponding  nitric  acid  is  unknown.  We  have  thus 
the  series:  O=PCL,  O=P(OH)S,  O=As(OH)o,  and 
0=Sb(OH)3. 

On  heating  these  bodies  the  elements  of  water  are  lost,  and 
the  "  meta-acids  "  are  formed;  at  a  temperature  of  about 
O 

200°,   O=P(OH)3  yields  P-OH,   and   O=As(OH)3, 

II 

O 
O 

II 

As  —  OH  ;    the    former    is    a    glass,    the    latter    a    pearly 
II 

O 

substance.  On  adding  water  to  metaphosphoric  acid 
it  dissolves  as  such,  and,  on  neutralisation,  it  yields  a 
series  of  metaphosphates  ;  but  metarsenic  acid,  when 
treated  with  water,  is  reconverted  into  orthoarsenic  acid  ; 
a  similar  change  can  be  produced  with  metaphosphoric 
acid,  but  only  after  prolonged  boiling. 

Dl=Acids.  —  We  are  unacquainted  with  any  normal  di- 
acid  of  this  group,  but  a  number  of  anhydrides  are  known. 
If  Z  stand  for  any  element  of  this  group,  the  series  should 
run  as  follows  :  — 

/OH  OH 


2= 

\OH  \OH 

Di-acid.  ist  Anhydride. 


PHOSPHORIC  ACIDS  125 

/OH  0=Z—  OH 

|  \ 

o  o 


=- 

\OH  O=Z—  OH 

2nd  Andryhide.  3rd  Anhydride. 

Neither  the  di-acid  nor  the  first  anhydride  are  known 
in  any  case,  but  the  second  anhydride,  which  is  generally 
called  the  "pyro"  acid,  because  it  is  formed  in  certain 
cases  by  heating  the  "  ortho  "  acid,  is  known  with  phos- 
phorus, arsenic,  antimony,  and  vanadium.  Pyrophos- 
plioric  acid  is  formed  at  215°;  but  the  change  is  not 
complete,  and  if  a  higher  temperature  be  employed  the 
meta-acid  is  also  produced.  Pyroarsenic  acid  is  formed 
by  heating  the  ortho-acid  to  140°-!  60°.  Pyroantimonic 
acid,  however,  is  best  prepared  by  the  action  of  boiling 
water  on  antimonyl  chloride,  O=SbCl3  ;  the  ortho-acid, 
which  is  probably  formed  first,  loses  the  elements  of  water, 
forming  the  pyro-acid,  H2Sb2O7.  Pyro-phosphoric  acid 
is  a  syrupy  glass-like  substance  ;  pyro-arsenic  acid  forms 
hard  crystals,  and  pyro-antimonic  acid  is  a  sparingly  soluble 
white  powder. 

Basicity.  —  The  basicity  of  these  acids  is  deduced  from 
the  formulas  of  double  salts.  Thus,  there  are  three  ortho- 
phosphates  of  sodium  and  hydrogen  ;  they  have  the 
formulae  H2NaPO4,  HNa2PO4,  and  Na3PO4  ;  the  hydro- 
gen calcium  salts  are:  H4Ca(PO4)9,  HCaPO4,  and 
Ca3(PO4)2.  It  is  therefore  argued  that  since  the  hydro- 
gen atoms  of  ortho-phosphoric  acid  are  replaceable  in  three 
stages  by  metals,  there  are  therefore  three  atoms  of  hydro- 
gen. These  salts  are  made  by  mixture  ;  2HHPO4.Aq  + 
Na3PO4.Aq  =  3H2NaPO4.Aq,  and  so  on.  The  acid  is, 
therefore,  said  to  be  tri-basic.  The  arsenates  are  precisely 
similar  ;  but  only  simple  vanadates  are  known,  and  no 
ortho-antimonates.  A  pyrophosphate  is  known  of  the 
formula  HK2(NH4)P2O7,  which  demonstrates  the  tetra- 


126  MODERN   CHEMISTRY 

basic  character  of  pyrophosphoric  acid,  and  the  other 
pyro-acids  are  classified  accordingly. 

Metaphosphoric  Acids. — The  formula  of  the  third 
anhydride  of  the  di-acid,  H2Z.7O0,  given  on  the  pre- 
ceding page,  is  a  multiple  by  two  of  that  of  the  meta- 
acid,  and  it  is  evident  that  the  fourth  anhydride  of  the 
tri-acid,  the  fifth  of  the  tetra-acid,  and  so  on,  will  all 
be  multiples  of  the  simpler  formula  of  the  meta-acid. 
These  acids  and  some  of  their  salts  appear  to  be  known 
in  the  case  of  the  phosphoric  acids,  and  what  is  usually 
termed  "  meta-phosphoric  acid,"  and  given  the  formula 
HPO3,  is  probably  the  seventh  anhydride  of  hexa-phosphoric 
acid,  HrP6O18,  for  one  of  its  double  salts  has  the  formula 
Na2Ca5(P6018).2. 

Complex  salts  are  known  in  the  case  of  almost  all 
these  elements.  Among  such  compounds  are  :  H2N4O11, 
Ag6P4O13,  Ag12P10O31,  Na6Vf)O17 ;  while  niobates  and 
tantalates  are  particularly  prone  to  form  such  complex  salts. 
Compounds  of  a  complicated  kind,  too,  in  which  one  of 
these  elements  replaces  another  partially,  have  been  made  ; 
as  an  example,  K(.(P8V12)O60.2iH9O  may  be  instanced. 
They  are  made  by  mixture. 

The  source  of  the  nitrates  is  the  attack  of  ammonium 
salts  resulting  from  the  decomposition  of  urea  (the  chief 
form  in  which  all  animals  part  with  the  nitrogen  they 
absorb  as  a  constituent  of  their  food)  by  a  bacterium  named 
the  "  nitrate  ferment."  This  organism  exists  only  in  the 
dark  ;  it  is  an  inhabitant  of  the  soil,  and  causes  the  oxida- 
tion of  ammonia,  from  whatever  source,  into  a  nitrate.  As 
potash  and  lime  are  the  commonest  bases  in  the  soil,  nitrates 
of  potassium  and  calcium  are  the  chief  compounds  formed. 
Vast  tracts  of  country  in  Chili  and  Peru  contain  beds  of 
sodium  nitrate,  possibly  formed  by  the  attack  of  the  debris 
of  previous  generations  of  animal  organisms  by  the  nitrate 
ferment.  By  distilling  a  mixture  of  sodium  or  potassium 
nitrate  with  sulphuric  acid  in  glass  vessels,  or,  on  a  large 
scale,  in  iron  vessels  on  which  concentrated  nitric  acid  is 


PHOSPHORIC  ACIDS  127 

without  action,  nitric  acid  comes  over  into  the  receiver  : 
NaNO3  +  H2SO4  =  HNO3  +  HNaSO4.  It  is  not  econo- 
mical to  use  the  equivalent  quantity  of  sulphuric  acid,  for 
the  reaction  between  hydrogen,  sodium  sulphate,  and  sodium 
nitrate  takes  place  at  a  temperature  so  high  that  much  of 
the  nitric  acid  is  decomposed  :  4HNO3  =  2H.2O  +  4NO2 
+  O2.  Nitric  acid  is  a  colourless  fuming  liquid,  with 
very  corrosive  properties.  In  aqueous  solution  it  is  one  of 
the  strongest  acids,  for  it  is  highly  ionised.  It  is  also  a 
powerful  oxidising  agent ;  this  has  been  referred  to  on 
p.  97.  Its  anhydride,  N2O5,  is  produced  on  distilling 
a  mixture  of  nitric  acid  with  phosphoric  anhydride  ;  the 
distillate  separates  into  two  layers  ;  the  upper  one  consists 
mainly  of  N2O5,  and  the  anhydride  separates  in  crystals 
when  it  is  cooled  ;  the  lower  layer  contains  H0N4On,  a 
liquid  solidifying  at  -  5°  ;  it  is  the  last  anhydride  of  tetra- 
nitric  acid.  The  anhydride  decomposes  spontaneously  in  a 
few  days  into  the  peroxide,  N2O4,  and  oxygen. 

Nitrates. — The  nitrates  are  all  soluble  salts,  possess- 
ing the  colours  of  their  metallic  ions.  As  a  rule,  they 
crystallise  easily.  They  are  all  decomposed  by  heat ;  those 
of  the  metals  of  the  alkalies  into  nitrite  and  oxygen  ;  and 
all  others  into  the  oxide  of  the  metal  and  nitric  oxide  and 
peroxide,  NO  a^d  NO2.  They  are  formed  by  dissolving 
the  metal,  the  oxide,  or  the  carbonate  in  dilute  nitric  acid. 
All  metals  are  attacked  by  nitric  acid,  except  gold  and  the 
metals  of  the  platinum  group.  The  chief  nitrates  are  those 
of  potassium,  KNO3,  saltpetre  or  nitre  ;  of  sodium,  NaNO3, 
Chili  saltpetre  ;  ammonium  nitrate,  NH4NO3,  from  which 
nitrous  oxide,  N2O,  is  obtained  on  heating  ;  lead  nitrate, 
Pb(NO3)2,  and  silver  nitrate,  AgNO3,  still  known  by  its 
old  name  "  lunar  caustic, "  the  word  "  lunar  "  referring  to 
the  ancient  alchemical  connection  between  silver  and  the 
moon.  It  is  used  as  a  caustic  for  removing  growths  and 
warts  ;  metallic  silver  is  deposited,  blackening  the  place 
rubbed. 

Phosphates. — The  source  of  phosphoric  acid  and 


128  MODERN   CHEMISTRY 

the  phosphates  is  chiefly  calcium  phosphate,  Ca3(PO4)0, 
a  mineral  known  as  phosphorite,  and  A1PO4,  aluminium 
phosphate,  or  gibbsite.  Phosphoric  acid  is  produced  from 
phosphorite  by  heating  it  with  dilute  sulphuric  acid  ;  spar- 
ingly soluble  calcium  phosphate  is  formed,  while  ortho- 
phosphoric  acid  goes  into  solution.  The  solution,  on 
evaporation,  deposits  white  crystals  of  HgPO4  ;  the 
residual  liquor  deposits  crystals  of  H3PO4.H9O  ;  com- 
mercial or  "glacial  phosphoric  acid  "  is  a  mixture  of  both 
kinds.  Its  solution  contains  many  hydrogen  ions,  and  it 
is  therefore  a  strong  acid.  But,  inasmuch  as  phosphoric 

4-  + 

acid  can  ionise  in  three  ways,  into  3H  and  PO4,  into  2H 

+ 
and  HPO4,  and  into  H  and  H2PO4,  there  are  three  kinds 

of  anions.  The  first  of  these,  PO4,  are  present  in  very 
small  relative  amount;  the  second  and -third,  HPO4  and 

H9PO4,  are  relatively  much  more  numerous.  There  is  a 
state  of  balance  between  the  quantities  of  these  ions  present 
in  any  solution  ;  and  if,  for  example,  kations  of  calcium  or 
lead  or  silver  be  added  to  a  solution  of  phosphoric  acid,  or 
to  one  of  hydrogen  di-sodium  phosphate,  Na.2HPO4,  the 

PO4  ions  present  enter  into  combination  with  the  kations, 
forming  Cas(POJ,,  Pb3(PO4),,  or  Ag3PO4  ;  the  PO~4 

ions  are  increased  at  the  expense  of  the  HPO4  and  H9PO4 
ions,  and  the  solution  becomes  more  acid.  On  adding  an 
alkali,  e.g.  caustic  soda,  to  a  solution  of  phosphoric  acid, 
neutrality  occurs  when  the  salt  Na0HPO4  has  been  reached; 

+ 

the  ions  are  then  mainly  2Na  and  HPO4.  On  adding 
more  soda,  the  solution  becomes  alkaline,  indicating  the 

presence  of  free  OH  ions  ;   and  it  is  only  on  concentration 

_  _j- 

that  these  OH  ions  combine  with  the  few  H  ions  of  the 


PHOSPHATES  129 

+     +  --- 

ionised,  Na.2HPO4,  forming  non-ionised  water,  and  "  tri- 
basic  "  sodium  phosphate,  Na3PO4,  is  left  as  a  residue. 
Similar  remarks  apply  to  the  ortho-arsenates.  The 
ortho-vanadates  are  hydrolysed  by  water  into  pyro-  and 
meta-vanadates. 

The  chief  orthophosphates  are:  Na2HPO4.i2H2O, 
obtained  by  neutralising  phosphoric  acid  with  sodium  car- 
bonate ;  HNa(NH4)PO4.4H2O,  named  "  microcosmic 
salt";  the  human  organism  used  to  be  known  as  the 
"  microcosm,  "  and  this  salt  crystallises  out  of  concentrated 
urine  ;  Ca3(PO4)o,  prepared  by  precipitation,  and  found  native 

.Ca—  PO4=Ca 
as    phosphorite  ;    F—  Ca—  PO  /  ,   a   widely 

XCa-P04=Ca 

spread  mineral  termed  apatite;  (NH4)MgPO4.6H2O,  a 
white  precipitate  produced  by  adding  ammonium  and 

+ 
magnesium  ions  to  those  of  a  soluble  phosphate  :   (NHJ  + 

Mg  +  PO4=(NH4)MgPO4.  It  is  the  usual  test  for  the 
presence  of  magnesia,  and  serves  at  the  same  time  to  dis- 
tinguish phosphoric  acid  ;  arsenates  give  a  precisely  similar 
precipitate.  The  precipitate  is  nearly  insoluble  in  am- 
moniacal  water,  and  it  may  be  filtered  off  and  washed  with 
water  containing  ammonia  with  very  little  loss.  Like 
almost  all  phosphates,  it  is  soluble  in  water  containing 
hydrogen  ions  ;  and  by  the  addition  of  ammonium  hydr- 
oxide their  number  is  greatly  diminished.  On  ignition, 
it  yields  magnesium  pyrophosphate,  Mg2P0(X,  thus  : 

" 


Arsenates.  —  The  important  arsenates  correspond 
exactly  in  formula  and  crystalline  form  to  the  phosphates  ; 
the  only  striking  difference  is  in  the  colour  of  the  silver 
salt  ;  while  ortho-phosphate  of  silver  is  yellow,  the  ortho- 
arsenate  is  brick-red. 

Vanadates.  —  Ortho-vanadates  are  prepared  by  fusing 
vanadium  pentoxide  with  the  required  amount  of  a  carbonate; 


130  MODERN   CHEMISTRY 

on  addition  of  nitric  acid  to  one  of  its  salts,  metavanadic 
acid  separates  out  as  a  brown-red  powder  ;  on  ignition,  a 
sparingly  soluble  red  powder  is  left:  2HVO3  =  H.,O  + 
V2O5.  Ortho-antimonates  are  unknown. 

Thio- Acids. — TMo-compounds  are  known,  analogous 
to  these  salts.  Mention  may  be  made  of  mixed  oxy-thio- 
phosphates,  e.g.  Na3POgS  and  Na3POS3,  which  result 
from  the  action  of  alkaline  hydroxides  on  phosphorus  penta- 
sulphide,  a  grey  solid  produced  by  direct  combination  of  phos- 
phorus with  sulphur.  They  are  easily  decomposed  by  hot 
water ;  hence  the  thio-arsenates  and  the  thio-antimonates 
are  better  known.  Arsenious  sulphide,  As2S3,  a  yellow  pre- 
cipitate formed  by  the  action  of  hydrogen  sulphide  on  a  solu- 
tion of  arsenious  chloride,  and  antimony  trisulphide,  Sb9S3,  an 
orange  precipitate  similarly  formed,  dissolve  in  solutions  of  poly- 
sulphides  of  the  alkalies;  these  solutions,  on  evaporation,  deposit 
crystals  on  cooling  :  As2S3  =  2KjSJ.Aq  =  2K3AsS4.Aq  -f- 
S(n_2).  Sodium  thio-antimonate,  Na3SbS4.9H2O,  has  long 
been  known  as  "Schlippe's  salt."  One  of  the  sulphur  atoms 
may  be  replaced  by  selenium,  giving  Na3SbS3Se.9H0O, 
thus  showing  the  similarity  in  character  between  sulphur 
and  selenium. 

Pyrophosphoric  Acid. — When  hydrogen  di-sodium 
orthophosphate  is  heated  to  redness,  water  is  lost,  and 
tetra-sodium  pyrophosphate  is  left  as  a  white  deliquescent 
mass  :  2HNa2PO4  -  Na4P2Or  +  H2O.  This  salt  is  soluble 
in  water.  On  adding  to  it  lead  nitrate,  a  precipitate  of 
lead  pyrophosphate  is  thrown  down ;  it  is  filtered  off, 
suspended  in  water,  and  a  current  of  hydrogen  sulphide 
is  passed  through  the  liquid.  Lead  sulphide  is  formed, 
and,  on  removing  it  by  filtration,  the  solution  contains 
pyrophosphoric  acid.  With  silver  nitrate,  a  pyrophosphate 
gives  a  white  precipitate  of  silver  pyrophosphate,  a  reaction 
which  distinguishes  this  acid  from  orthophosphoric  acid, 
for  silver  orthophosphate  is  yellow.  Magnesium  pyro- 
phosphate has  already  been  alluded  to.  The  pyrophosphates 
of  the  metals,  those  of  the  alkalies  excepted,  are  insoluble 


MET  A-S  ALTS  131 

in  water,  but,  for  reasons  similar  to  those  given  in  describ- 
ing the  ortho  phosphates,  they  dissolve  in  acids. 

Pyroantimonate  of  potassium  is  a  salt  obtained  by 
fusing  the  metantimonate,  KSbO3,  with  caustic  potash, 
and  crystallisation  of  the  resulting  fused  mass  from  water. 
It  is  easily  soluble,  but  on  adding  its  solution  to  that  of  a 
sodium  salt,  a  precipitate  of  the  sparingly  soluble  di-hydrogen 
di-sodium  pyroantimoniate,  HgNagSb^CX,  is  produced,  It 
is  one  of  the  very  few  sparingly  soluble  salts  of  sodium. 

Meta*  Salts.  —  On  heating  to  redness  di-hydrogen 
sodium  orthophosphate,  H9NaPO4,  or  microcosmic  salt, 
H(NH4)NaPO4.4H2O,  water,  or,  in  the  latter  case, 
ammonia  in  addition,  is  lost,  and  the  residue  consists  of 
sodium  hexa-metaphosphate,  (NaPO3)6.  It  is  a  glass 
soluble  in  water  ;  its  salts  are  mostly  gelatinous.  The  acid, 
which  is  probably  also  hexa-metaphosphoric  acid,  is  a 
soluble  glass,  formed  on  igniting  ortho-phosphoric  acid ; 
it  yields  salts  like  that  mentioned  on  p.  126.  Unlike  the 
other  two  phosphoric  acids,  it  coagulates  a  solution  of 
\vhite-of-egg  or  albumen  in  water.  Its  silver  salt  is  white 
and  gelatinous.  Mono-metaphosphates  are  insoluble  salts, 
produced  by  igniting  together  oxides,  carbonates,  sulphates, 
or  nitrates  with  excess  of  phosphoric  acid,  and  removing 
the  excess  of  phosphoric  acid  with  water.  The  salts  of 
the  alkalies  are  sparingly  soluble.  Metarsenates  are  pro- 
duced in  a  similar  manner  to  the  hexa-metaphosphates,  but, 
on  treatment  with  water,  they  combine  with  water  and 
re-form  the  orthoarsenates  of  metal  and  hydrogen  from 
which  they  were  obtained.  Some  pyro-  and  meta-thio- 
arsenates  have  been  prepared. 

Compounds  containing  less  Oxygen.  —  The 
elements  of  the  nitrogen  group  are  characterised  by  their 
possessing  more  than  one  valency.  They  are  also,  in 
most  cases,  capable  of  forming  compounds  with  hydrogen. 
These  two  characteristics,  taken  together,  lead  to  the 
possibility  of  their  forming  a  number  of  isomeric  com- 
pounds, i.e.  compounds  having  an  identical  composition, 


132  MODERN   CHEMISTRY 

but  being,  at  the  same  time,  different  chemical  individuals. 
Some  such  compounds  are  known,  at  least  in  their  de- 
rivatives. The  conception  will  be  clearer  after  inspection 
of  the  following  table  : — 

HOX   /OH   HO,   /H    HOv   /H    HO-.   /H 

HO7  NOH   HO/  \OH   HO/  \DH   HO/ 

(i)          (2)  (3)         (4) 

/OH        /H          /H          /H 

\OH        \OH        \OH        \H 

(9)          (10)          (ii)          12) 

/OH         /H 
(15)          (16) 


/OH  /H  /H  /H 

N(-OH  Nr-OH  N^H  N^-H 

\OH  X)H  XOH  \H 

(5)  (6)  (7)  (8) 

/OH  /H 


(13)         (14) 

For  convenience'  sake,  the  compounds  have  been  written 
as  derivatives  of  nitrogen,  but  the  type  is  followed  by  other 
elements  of  the  group. 

(  i  )  is  the  true  "  ortho  "  acid,  unknown  in  all  cases. 
(9)  is  its  first  anhydride,  known  in  "  orthophosphoric  " 
acid  and  in  "  orthoarsenic  "  acid.  (IS)  is  nitric  acid, 
and  corresponds  to  mono-metaphosphoric  acid,  metavana- 
dic  acid,  the  metarsenates,  and  the  metantimonates.  (2) 
and  (10)  are  unknown  bodies,  but  (10)  corresponds  to 
phosphorous  acid,  and  (16)  to  the  nitrites.  (3)  is  also 
unknown,  but  (  1  1  )  is  represented  by  hypophosphorous  acid 
and  the  hypophosphites.  (4)  is  unknown.  (I2)>  how- 


PHOSPHOROUS  ACID  133 

ever,  may  possibly  be  the  formula  of  hydroxylamine ;  its 
name,  in  that  case,  should  be  "  oxy-ammonia."  In  all 
these  compounds  the  element  is  a  pentad.  The  other 
compounds  contain  triad  element.  ( 5  )  probably  represents 
the  formulae  of  the  arsenites  ;  (  1 3 )  is  an  alternative  formula 
for  nitrites.  (6)  and  (14)  are  unknown.  (7)  is  an  alter- 
native formula  for  hydroxylamine. 

Phosphorous  Acid. — We  shall  first  consider  numbers 
(8)  and  (16).  In  phosphorous  trichloride,  PC13,  phos- 
phorus is  undoubtedly  a  triad.  On  heating  this  compound 
to  60°,  and  passing  over  it  a  current  of  dry  air,  and  subse- 
quently leading  the  air  through  ice-cold  water,  crystals 
separate,  which  are  washed  with  ice- water  and  dried  in 
a  vacuum.  They  have  the  formula  H3PO3.  The  acid, 
however,  is  di-basic  ;  the  formula  of  its  sodium  salt,  for 
example,  is  Na.2HPO3.  Again,  phosphorous  anhydride 
P4O6,  produced  by  the  combustion  of  phosphorus  in  a 
limited  supply  of  air,  constitutes  a  crystalline  substance, 
melting  at  22.5°  ;  it  is  acted  on  only  very  slowly  by  cold 
water,  and  then  yields  phosphorous  acid.  These  facts  point 
to  a  molecular  change  from  P(OH)3  to  O=PH(OH)2. 
But  this  view  is  rendered  certain  by  consideration  of  the 
ethyl  salts  of  the  acids. 

Constitution  of  Phosphorous  Acid. — Phosphorous 
trichloride,  if  treated  with  a  solution  of  sodium  ethoxide, 
Na(OC.->H-)o,  in  alcohol,  yields  tri-ethyl  phosphite, 
(C,H5)3PO?~  or  P(OC2H5)3,  corresponding  to  P(OH)g. 
It  is  a  liquid,  boiling  at  191°.  On  the  other  hand,  a 
compound  analogous  to  hydrogen  phosphide,  PH^,  is 
known,  of  the  formula  PH2(C2H5),  named  di-ethyl 
phosphine,  which,  on  oxidation,  yields  a  di-basic  acid 
analogous  to  phosphorous  acid,  O=P(C2H5)(OH)0,  named 
ethyl-phosphinic  acid,  from  which  the  ethyl  salt  can  be 
prepared,  C-P(C2H5)  (OC2H5)2,  isomeric  with  ethyl 
phosphite.  Ethyl  phosphite  is  a  derivative  of  triad  phos- 
phorus, whereas  di-ethyl  ethyl-phosphinate  is  derived  from 
pentad  phosphorus.  The  anhydride  of  phosphinic  acid, 


134  MODERN   CHEMISTRY 

O 

II 

O=PH(OH)2,  would  be,  not  P2O3,  but  H-P=O,  like 
(16).  But  this  substance  is  not  formed  on  heating  phos- 
phorous acid,  for  it  decomposes  into  phosphoric  acid  and 
phosphoretted  hydrogen,  thus:  4HgPO3  =  PHg  +  3H3PO4. 
One  of  the  varieties  of  the  salts  of  nitrous  acid,  however, 
has  a  corresponding  formula. 

Nitrites. — When  a  nitrate  of  one  of  the  metals  of  the 
alkalies  is  heated  with  metallic  lead,  lead  monoxide  is 
formed,  and  a  nitrite,  thus  :  KNO3  +  Pb  =  PbO  +  KNO2. 
The  nitrite  is  left  as  a  white  fusible  salt,  easily  soluble  in  water. 
On  acidifying  a  very  dilute  solution  with  sulphuric  acid,  a 
dilute  solution  of  nitrous  acid  is  formed  ;  but  on  warming  it, 
a  somewhat  complex  action  takes  place.  First,  the  anhy- 
dride is  produced :  2HNO9.Aq  =  H9O.Aq  +  N9O3  ;  next, 
the  anhydride  is  attacked  by  the  water  and  decomposed  : 
3N^O3  +  H.2O  =  2HNO3  +  4NO  ;  and  some  of  the  anhy- 
dride volatilises  with  decomposition  into  nitric  oxide  and 
peroxide  :  N0O3  =  NO  +  NO9.  The  nitrites  are  white, 
easily  soluble  crystalline  salts  ;  those  of  lead,  Pb(NO9)9, 
and  silver,  AgNO9,  are  sparingly  soluble.  All  are  decom- 
posed by  the  stronger  acids  ;  for  nitrous  acid  is  a  weak  acid, 
and,  moreover,  it  is  easily  decomposed,  as  has  been  pointed 
out.  None  of  these  changes  throws  any  light  on  the  constitu- 
tion of  nitrous  acid,  however.  To  gain  this  knowledge  it  is 
necessary  to  study  the  alkyl  salts  ;  for  example,  ethyl  nitrite. 

Constitution  of  the  Nitrites.  —  Ethyl  nitrite, 
made  by  distilling  together  a  mixture  of  sodium  nitrite, 
sulphuric  acid,  and  alcohol,  is  a  volatile  colourless  liquid 
with  a  fragrant  odour.  On  boiling  it  with  a  solution  of 
sodium  hydroxide  it  is  hydrolysed,  the  ethyl  group  being 
again  replaced  by  the  metal  sodium,  thus  :  O=N— O(C9H5) 
+  NaOH.Aq  =  O=N-ONa.Aq  +  C2H5OH.  And  if 
ethyl  nitrite  be  placed  in  a  flask  along  with  tin  and  hydro- 
chloric acid — in  other  words,  exposed  to  the  action  of 
nascent  hydrogen — the  products  are  ammonia  (with  some 


NITRITES  135 

H  H     H 

hvdroxylamine)  and  alcohol  :   O  =  N-HorO  +  N-H  + 


HO(C.,H5).      Sodium  nitrite  therefore  appears  to  possess 
the  formula  O=N—  ONa.       But  silver  nitrite,  heated  in  a 
sealed  tube  with  ethyl  iodide,  yields  a  compound  of  the 
same  composition  as,  but  not  identical  with,  ethyl  nitrite, 
O 
II 

and  the  formula  N—  (C.2H5)  is  ascribed  to  it  ;   for,  on  heat- 
II 

O 

ing  with  caustic  soda,  it  is  not  hydrolysed,  but  one  of  the 
atoms  of  hydrogen  of  the   ethyl   group   is  replaced  by  the 
O 
II     • 

element  sodium,  giving  N—  (C.?H4Na)  ;   and  further,  with 
II 

O 

nascent  hydrogen,  the  two   atoms  of  oxygen  are  removed 
and  replaced  by  hydrogen,  yielding  ethylamine,  a  compound 
H 

analogous  to  ammonia,  N—  (C0H5)  ;    this   shows    that  the 

H 

ethyl  group  in  the  compound,  which  is  named  nitroethane, 
is  in  direct  union  with  the  nitrogen  atom.     It  appears,  then, 

O 

II 

that    silver    nitrite    has    the    formula    N—  Ag,    and     not 

6 

O=N—  OAg.       It    also    follows    that    two    nitrous    acids 

O 

il 
must   exist,   O=N—  OH    and   N—  H,  the    former    (13)    a 

II 
O 


136  MODERN   CHEMISTRY 

derivative  of  triad,  and  the  latter  (16)  of  pentad  nitrogen. 
But  the  acids  are  unknown,  and  it  is  only  possible  to  guess 
the  constitutional  formulae  of  the  salts  through  the  reactions 
just  described. 

Arsenites.  —  Arsenites,  derived  from  the  acid 
HgAsOg,  such  as  hydrogen  cupric  arsenite  or  "  Scheele's 
green,"  HCuAsO3,  produced  by  adding  to  a  solution  of 
copper  sulphate  potassium  arsenite,  arsenious  oxide,  and  a 
little  ammonia ;  pyro-arsenites,  such  as  K4As9O5,  and 
metarsenites,  KAsO9  ;  also  ortho-  and  meta-thioarsenites, 
K3AsSg  and  KAsS9,  are  known.  They  show  no  signs  of 
isomerism  like  that  of  the  phosphites  and  nitrites,  and  they 
are  doubtless  salts  of  As(OH)3  and  O=As— OH,  and 
the  corresponding  sulphur  acids,  although  the  acids  corre- 
sponding to  the  sulphur  salts  are  unknown.  Metantimonite 
of  sodium,  NaSbO9,  and  metarthioantimonite,  NaSbS9,  are 
formed  by  dissolving  antimonious  oxide,  Sb4O6,  or  the  sul- 
phide, Sb9S3,  in  caustic  soda,  and  precipitating  with  alcohol. 

Hypophosphites. — Hypophosphorous  acid,  H3PO2, 
is  a  monobasic  acid  ;  sodium  hypophosphite  has  the  formula 
Na(H9PO9).  This  leads  to  a  formula  analogous  to  that 
given  in  ( 1 1 ) .  When  heated,  too,  the  acid  yields  phosphine 
and  phosphoric  acid:  2HgPO2  =  PH3  +  HgPO4.  This 
would  lead  to  the  supposition  that  some  of  the  hydrogen 
was  already  in  combination  with  the  phosphorus.  Its  salts 
also  yield  phosphine,  together  with  a  phosphate  and  free 
hydrogen.  The  acid  is  prepared  by  the  action  of  sulphuric 
acid  on  the  barium  salt ;  that  salt  is  prepared  by  boiling 
together  yellow  phosphorus  and  caustic  baryta  :  2P4 
+  3Ba(OH)9.Aq  +  6H2O  =  2PH3  +  3Ba(H2PO2)2.Aq. 
With  sulphuric  acid  insoluble  barium  sulphate  is  formed, 
while  hypophosphorous  acid  remains  in  solution.  It  forms 
white  crystals,  melting  at  17.4°.  The  acid  has  reducing 
power  ;  with  silver  nitrate,  for  example,  metallic  silver  is 
precipitated  and  phosphoric  acid  is  formed.  With  hydrogen 
iodide  phosphorous  acid  and  phosphonium  iodide  are  formed : 
3H(H2P02)  +  HI  =  2H2(HP03)  +  PH4I. 


HYPOPHOSPHATES  137 

Two  acids  are  known  belonging  to  this  group  of  ele- 
ments ;  they  have  not  been  tabulated  on  p.  132,  because 
their  structure  may  be  compared  with  that  of  hydrazine  or 
liquid  phosphine,  H2N—  NH2  or  HaP—  PH2,  in  which  two 
atoms  of  nitrogen  —  or  of  phosphorus  —  are  in  direct  union 
with  each  other.  These  are  phosphatic  acid,  or,  as  it  is 

0=P=(OH)2 

sometimes  termed,  hypophosphoric  acid,         I  , 

0=P=(OH)2 

N-(OH) 
and  hyponitrous  acid,   II  .     The  first  of  these  is 

N-(OH) 

produced  in  small  quantity  along  with  ortho-phosphoric  and 
phosphorous  acids,  when  phosphorus  is  oxidised  by  exposure 
to  moist  air.  It  is,  however,  best  made  from  its  silver  salt, 
by  addition  of  the  equivalent  quantity  of  hydrochloric  acid. 
Silver  hypophosphate  is  produced  by  dissolving  6  grams  of 
silver  in  100  grams  of  nitric  acid  diluted  with  its  own 
weight  of  water,  and  adding  to  the  solution,  warmed  on  a 
waterbath,  8  or  9  grams  of  phosphorus.  As  soon  as  the 
violent  evolution  of  nitrous  gases  ceases  the  liquid  is  cooled, 
and  silver  hypophosphate  crystallises  out.  The  acid  has 
no  reducing  properties,  hence  it  probably  contains  no  hydro- 
gen capable  of  conversion  into  hydroxyl  by  the  addition  of 
oxygen.  The  sodium  salt,  Na4P2O6,  is  converted  into 
pyrophosphate  by  the  action  of  a  solution  of  bromine  in 
water  ;  the  change  is  evidently  due  to  the  addition  of 

" 


oxygen,  thus  :  +  O  =       O  .      The 

0=P=(OH)2 


anhydride  of  this  acid  would  be  ;   a  compound  of 

0=P=0 

the  formula  P2O4  is  produced  by  the  incomplete  combustion 
of  phosphorus  in  oxygen  ;   but  as  it  yields  orthophosphoric 


138  MODERN   CHEMISTRY 

and  phosphorous  acids  on  treatment  with  water,  it  is  in  all 

O 
probability  phosphoryl  phosphate,  O=P~O~P\\     . 

X^o 

Hyponitrites  are  produced  by  the  action  of  sodium 
amalgam,  that  is,  a  solution  of  sodium  in  mercury  contain- 
ing about  4  per  cent,  of  the  former,  on  a  solution  of  potas- 
sium or  sodium  nitrite.  After  the  mixture  has  stood  for 
some  days,  it  is  rendered  slightly  acid  with  acetic  acid,  and 
silver  nitrate  is  added.  A  yellow  precipitate  of  silver 
hyponitrite  is  produced  ;  other  hyponitrites  may  be  pre- 
pared from  it  by  the  addition  of  the  calculated  quantity  of 
the  respective  chloride.  The  acid  can  also  be  liberated  by 
the  addition  to  a  very  dilute  aqueous  solution  of  the  equiva- 
lent amount  of  hydrochloric  acid.  On  warming  the  solution 
of  the  acid,  nitrous  oxide  is  evolved  ;  but  nitrous  oxide 
does  not  unite  with  water  to  form  the  acid. 

That  the  acid  has  the  formula  HL,N2O0,  and  not  HNO, 
is  shown  by  its  formation  from  hydroxylamine  and  nitrous 
acid.  On  mixing  dilute  solutions  of  hydroxylamine  sulphate 
and  sodium  nitrate,  the  hydroxylamine  nitrate  loses  water, 
thus:  HO-NH2  -i-  O=N-OH  =  H2O  +  HO-N=N-OH; 
the  silver  salt  is  thrown  down  on  addition  of  silver  nitrate. 


CHAPTER   VIII 

The  Oxy= Acids  of  the  Halogens ;  Perchlorates  and 
Periodates ;  Chlorates,  Bromatest  and  lodates; 
Chlorites ;  Hypochlorites,  Hypobromites,  and 
Hypoiodites— Acids  and  Salts  of  Sulphur,  Sele- 
nium, and  Tellurium ;  of  Molybdenium,  Tung* 
sten,  and  Uranium — Perchromates,  Persulphates, 
Perborates,  and  Percarbonates. 

THE  formulae  of  the  acids  of  the  halogens  present  some 
analogy  with  those  of  the  nitrogen  group,  for,  like  the 
latter,  the  halogens  also  possess  uneven  valency.  But  while 
the  highest  valency  of  elements  of  the  nitrogen  group  is 
that  of  a  pentad,  chlorine  and  iodine  function  as  heptads  in 
perchloric  and  periodic  acids.  The  valency  of  the  halogens 
is  five  in  chloric,  bromic,  and  iodic  acids  ;  three  in  chlorous 
acid  ;  and  one  in  the  hypochlorites,  hypobromites,  and 
hypoiodites.  A  short  table,  analogous  to  that  given  on 
p.  132,  shows  the  relation  between  these  compounds  : — 

I(OH)6(ONa),    corresponding    to    I(OH)T,   ortho- 

periodates  ; 
O=I(OAg)5,    corresponding    to   O=I(OH)5,  para- 

periodates  ; 

°\  °\ 

/^I(OAg)3,  corresponding  to       \I(OH)g,  meso- 

( middle)  periodates  ; 

139 


MODERN  CHEMIST'RY 


°\ 

O^I(OAg),  corresponding   to    O^I(OH),  meta- 


periodates. 

^° 

~-=rI—  O—  Is=O,  unknown  periodic  anhydride. 


Perchloric  acid,  O3C1(OH),  corresponding  to  meta- 
periodic  acid,  is  the  only  representative  of  these  among 
the  other  members  of  the  halogen  group.  But  the 
periodates,  like  the  phosphates,  form  still  more  condensed 
acids  ;  thus,  salts  of  a  di-ortho-periodic  acid,  H8I2O1;L, 
and  of  a  di-meso-periodic  acid,  H4I2O9,  as  well  as  of  a 
tetra-  and  hexa-periodic  acid,  H10I4O19  and  H0()I6O01, 
are  known. 

T(OH)5,  ortho  iodic  acid;  orthobromic  and  ortho 
chloric  acids  are  unknown. 

O=I(OH)3,  and  similar  bromine  and  chlorine  acids,  are 
unknown. 

O^  O^  O^ 

J^I(OH),       iBr(OH),  and      ^Cl(OH),   iodic, 

bromic,  and  chloric  acids. 

°\         SQ 

\\  —  O  —  1\\      ,    iodic   anhydride,    is    the    only    an- 

O^  ^O 

hydride  known. 

A  tri-iodic  acid,  HI3Og,  has  been  prepared. 

O=C1—  (OH),  chlorous  acid,  is  the  only  representative 
of  triad  halide. 

I-(ONa),  Br-(ONa),  and  Cl-(ONa),  hypoiodite, 
-chlorite,  and  -bromite  of  sodium  and  of  some  other 
metals  are  fairly  stable  in  solution. 

//ypoc/i/or/tes.  —  The  starting-point  for  these  com- 
pounds is  the  hypohalite  ;  it  is  produced  by  the  action  of  a 
hydroxide  on  the  element  in  cold  aqueous  solution,  thus  : 


HYPOCHLORITES  *  141 

2NaOH.Aq  +  Cl.>,  Br0,  or  I,  =  NaCl,  NaBr,  or  Nal.Aq 
+  H,O  +  NaOCl,"  NaOBr,  or  NaOI. Aq. 

Chlorine  monoxide,  C19O,  is  formed  on  passing 
over  dry  mercuric  oxide,  prepared  by  precipitation  from 
mercuric  chloride  with  caustic  soda,  dry  chlorine  gas  ;  the 
tube  containing  the  oxide  must  be  cooled  with  ice,  for  the 
monoxide  is  a  dark  brown,  very  unstable  liquid,  boiling 
at  6°.  The  equation  is:  2HgO  +  2C12  =  Hg2Cl2O  + 
Cl— O— Cl.  Its  density  at  10°  corresponds  with  the  formula 
given.  If  the  mercuric  oxide  be  made  into  an  emulsion 
with  water,  and  chlorine  be  passed  through,  the  acid  is 
produced  in  aqueous  solution  ;  it  is  a  pale  yellow  liquid, 
with  a  not  unpleasant  smell,  recalling  that  of  chlorine.  If 
concentrated,  it  decomposes  into  water,  chlorine,  and  oxygen. 
It  reacts  at  once  with  hydrochloric  acid,  forming  water  and 
chlorine :  H-O-C1. Aq  +  H-Cl.Aq  -  C12  +  H9O.Aq. 

The  most  important  hypochlorite  is  a  double  compound, 
obtained  by  the  action  of  chlorine  on  slaked  lime,  termed 
"chloride  of  lime"  or  " bleaching-powder."  It  is  a 
white,  non-crystalline  powder,  smelling  of  hypochlorous  acid. 
Its  formula  is  Cl— Ca— O— Cl.  That  it  is  a  compound,  and 
not  a  mixture  of  calcium  chloride  and  hypochlorite,  is 
proved  by  the  fact  that  bleaching-powder  is  not  deliquescent, 
whereas  calcium  chloride  is  a  very  deliquescent  salt;  calcium 
chloride  and  hypochlorite  are  both  very  soluble  salts,  but 
bleaching-powder  is  only  sparingly  soluble,  but  if  a  saturated 
solution  of  bleaching-powder  be  cooled,  crystals  of  hypo- 
chlorite separate  out,  thus  proving  that  it  is  dissociated  in 
aqueous  solution  into  these  two  salts.  Its  smell,  as  well  as 
that  of  other  hypochlorites,  is  due  to  the  fact  that  hypo- 
chlorous  acid  is  a  very  feeble  acid,  and  is  only  slightly 
ionised ;  hence  the  calcium  and  other  salts  are  hydrolysed 
by  the  ions  of  water,  and  the  solution  contains  free  base 
and  free  acid ;  and  the  latter  reveals  its  presence  by  its  smell. 
No  ion  has  a  smell ;  hence  one  does  not  smell  solutions  of 
salts,  but  only  volatile  non-ionised  compounds. 

When   bleaching-powder   is   distilled    with    just   enough 


i42  MODERN   CHEMISTRY 

acid  to  liberate  the  hypochlorous  acid,  that  acid  comes  over  ; 
but  if  excess  of  such  an  acid  as  sulphuric  or  hydrochloric 
be  added,  chlorine  is  liberated,  owing  to  the  reaction 
between  hydrochloric  and  hypochlorous  acids.  The  addition 
of  a  trace  of  a  salt  of  cobalt  to  bleaching-powder  results  in 
the  liberation  of  oxygen  when  it  is  warmed  ;  this  reaction, 
which  is  termed  "  catalytic,"  is  supposed  to  be  due  to  the 
alternate  formation  and  decomposition  of  an  oxide  of  cobalt 
of  the  formula  Co4O7 ;  but  the  reaction  is  still  obscure. 
The  bleaching  action  of  bleaching-powder  in  presence  of 
acid  is  ascribed  to  the  liberation  of  oxygen,  and  the  oxida- 
tion thereby  of  the  insoluble  brownish  colouring  matter  of 
unbleached  cotton  or  linen  to  soluble  compounds  which  can 
be  removed  by  washing. 

Chlorates.  —  Hypochlorites,  when  heated,  undergo 
conversion  into  a  mixture  of  chlorate  and  chloride : 
3NaOCl.Aq  =  NaClO3.Aq  +  2NaCl.Aq.  The  usual 
method  of  preparing  chlorates,  however,  is  to  pass  a  current 
of  chlorine  through  hot  "milk  of  lime" — that  is,  calcium 
hydroxide  suspended  and  partially  dissolved  in  water. 
Potassium  chloride  equivalent  to  one-sixth  of  the  lime  is 
also  present.  The  following  reaction  occurs:  6Ca(OH)2.Aq 
+  2KC1.  Aq  +  6C12  =  6CaCl2.  Aq  +  2KClOg.  Aq  +  6H2O. 
On  evaporation,  the  sparingly  soluble  potassium  chlorate  de- 
posits in  crystals,  leaving  the  very  soluble  calcium  chloride  in 
solution.  The  potassium  chlorate  is  purified  by  recrystallisa- 
tion.  It  is  a  white,  lustrous  salt,  crystallising  in  flat  plates. 
It  fuses  readily,  and,  at  a  somewhat  higher  temperature  than 
its  melting-point,  it  evolves  oxygen.  At  the  same  time  some 
of  the  chlorate  is  oxidised  by  the  oxygen,  and  perchlorate 
is  formed:  2KC1(X  =  2KC1  +  30,,  and  KCKX  +  O  = 
KC104. 

Perchlorates. — On  ceasing  to  apply  heat,  therefore, 
after  the  salt  has  become  pasty,  and  treating  with  water, 
the  potassium  chloride  is  dissolved,  leaving  the  much  less 
soluble  perchlorate ;  the  perchlorate  may  be  purified  by 
recrystallisation. 


CHLORINE   PEROXIDE  143 

Owing  to  the  fact  that  very  few  potassium  salts  are 
insoluble  in  water,  it  is  not  convenient  to  prepare  chloric 
acid  from  the  potassium  salt ;  for  this  purpose  it  is 
better  to  use  the  barium  salt,  made  from  baryta-water 
and  chlorine  ;  a  solution  of  this  salt,  when  mixed  with 
the  equivalent  amount  of  dilute  sulphuric  acid,  yields  a 
precipitate  of  barium  sulphate,  and  chloric  acid  remains  in 
solution. 

Chlorine  Peroxide. — The  solution,  freed  from  barium 
by  filtration,  may  be  concentrated  by  distilling  away  the 
water  at  a  low  temperature  in  a  vacuum  ;  the  acid  remains 
as  a  colourless,  syrupy  liquid,  which  decomposes  at  100° 
into  perchloric  acid,  water  and  chlorine  peroxide,  CIO.,  ; 
the  last  compound  is  unstable  at  that  temperature,  and 
explodes  into  chlorine  and  oxygen.  But  the  peroxide  may 
be  prepared  by  warming,  not  above  40°,  a  mixture  of  potas- 
sium chlorate  and  concentrated  sulphuric  acid  ;  the  chloric 
acid  decomposes  as  it  is  formed:  3HC1O3  =  HC1O4  + 
H2O  +  2C1O2.  It  is  a  dark  red  liquid,  boiling  at  10.6° 
to  a  reddish-brown  gas.  Unlike  nitric  peroxide,  it  does 
not  form  double  molecules ;  C19O4  is  unknown.  It  re- 
sembles that  compound,  however,  in  its  action  on  water  ; 
while  nitric  peroxide  gives  a  mixture  of  nitrous  and  nitric 
acids,  chlorine  peroxide,  added  to  an  alkali,  forms  a  chlorite 
and  a  chlorate  :  2C1O2  +  iKOH.Aq  =  KClO9.Aq  + 
KClO3.Aq. 

The  chlorates,  like  the  nitrates,  are  all  readily  soluble 
in  water  ;  lead  and  silver  chlorites,  like  the  corresponding 
nitrites,  are  sparingly  soluble  salts  ;  and  lead  perchlorate  is 
the  only  salt  which  does  not  easily  dissolve.  As  already 
mentioned,  chloric  acid  is  readily  decomposed  when  its 
aqueous  solution  is  warmed  ;  chlorous  acid  is  still  less 
stable  ;  but  perchloric  acid,  which  may  be  prepared  by 
distilling  together  potassium  perchlorate  with  concentrated 
sulphuric  acid,  is  relatively  stable,  seeing  that  it  can  be 
distilled  without  decomposition.  It  is  an  oily  liquid,  with 
acid  taste  ;  it  is  apt  to  explode  when  brought  into  contact 


144  MODERN   CHEMISTRY 

with  any  oxidisable  matter.     The  corresponding  perbromic 
acid  is  unknown. 

Hypobromites. — Hypobromites  are  produced,  along 
with  bromides,  on  mixing  solutions  of  alkalies  with  bromine ; 
the  solution  turns  yellow,  and  acquires  a  smell  like  that  of 
seaweed.  On  warming,  a  change  analogous  to  that  suffered 
by  hypochlorites  occurs  ;  the  hypobromite  yields  bromide 
and  bromate,  and  the  latter  can  be  separated  by  crystal- 
lisation. 

Bromates. — The  bromates  are  white  salts  soluble  in 
water ;  they  do  not,  however,  decompose  into  bromide  and 
perbromate  when  heated ;  the  perbromate  is  unstable,  and 
bromide  and  oxygen  are  the  only  products.  Bromic  acid, 
too,  when  warmed  changes  to  water,  hydrobromic  acid, 
bromine,  and  oxygen  ;  as  no  compound  analogous  to  C1O2 
is  produced,  bromous  acid  is  unknown. 

Hypoiodites.  —  The  formation  of  hypoiodites  is 
analogous  to  that  of  hypochlorites ;  but  the  salts  are 
known  only  in  solution  mixed  with  iodide.  Again,  like 
the  hypochlorites,  they  change  on  heating ;  they  yield  a 
mixture  of  iodide  and  iodate  ;  and  from  barium  iodate 
iodic  acid  can  be  prepared.  But  it  is  more  readily  obtained 
by  boiling  iodine  with  nitric  acid  ;  for  iodine  is  more  easily 
oxidised  than  either  chlorine  or  bromine ;  or  chlorine  and 
water  may  be  used  as  an  oxidising  agent. 

Iodic  Acid. — Iodic  acid  is  a  white  crystalline  com- 
pound, easily  soluble  in  water  ;  it  is  a  strong  acid,  and  its 
salts  are  produced  by  neutralisation  with  hydroxides  or 
carbonates.  When  it  is  mixed  in  solution  with  hydriodic 
acid,  mutual  decomposition  ensues  and  iodine  is  liberated : 
HI03.  Aq  +  sHI.  Aq  =  3 12  +  3H20.  Aq. 

Periodic  Acid.  —  The  oxidation  of  iodic  acid  to 
periodic  acid  is  accomplished  by  means  of  a  solution  of 
sodium  hypochlorite ;  it  is  easier  to  dissolve  iodine  in  a 
solution  of  sodium  carbonate,  when  hypoiodite  is  formed, 
and  to  saturate  the  solution  with  chlorine.  The  iodate  at 
first  formed  is  converted  into  the  periodate  :  NaIOg.Aq-f- 


THERMAL   DATA  145 

NaOCl. Aq  =  NaCl. Aq  +  NaIO4<  Aq.  As  the  periodate  is 
sparingly  soluble  in  water,  it  crystallises  out  on  concentrat- 
ing the  solution.  On  mixing  the  solution  of  the  sodium 
salt  with  silver  nitrate,  tri-hydrogen  di-argentic  periodate 
is  precipitated  ;  it  is  dissolved  in  hot  dilute  nitric  acid  and 
evaporated,  when  mono-argentic  periodate,  AgIO4,  crystal- 
lises out.  On  mixing  with  water,  this  salt  undergoes  the 
change  :  2AgIO4  +  4H?O  =  H8Ag2IO6  +  H5IO6.Aq. 
The  silver  salt,  which  is  insoluble  in  water,  is  removed  by 
filtration,  and  the  periodic  acid  deposits  in  crystals  on 
evaporation.  The  acid  forms  white  prisms  ;  on  heating  it 
to  130°,  it  decomposes  into  iodine  pentoxide,  I2O5,  a 
white  solid,  also  produced  on  heating  iodic  acid  to  170°, 
together  with  water  and  oxygen  ;  at  1 80°  the  pentoxide 
decomposes  slowly  into  iodine  and  oxygen. 

Thermal  Data. — From  the  short  description  which 
has  been  given,  it  is  seen  that  the  oxides  of  iodine  and  their 
compounds  are,  as  a  rule,  more  stable  than  those  of  bromine 
and  chlorine,  and  this  is  connected  with  the  heat  which  is 
evolved  or  absorbed  during  their  formation.  This  heat  is 
seldom  determined  directly ;  never  when  the  compounds 
are  produced  with  absorption  of  heat.  Thus,  when  chlorine 
combines  with  oxygen  to  form  C1.,O,  enough  heat  is  ab- 
sorbed to  cool  17,800  grams  of  water  through  i°,  or  what 
is  the  same  thing,  on  decomposing  C12O  heat  enough  is 
liberated  to  raise  the  temperature  of  17,800  grams  of 
water  through  i°.  This  is  termed  the  heat  of  formation 
of  the  substance.  The  heat  of  formation  of  chloric 
acid  from  chlorine,  oxygen,  and  water  involves  a  heat- 
absorption  of  20,400  calories,  and  these  substances  are 
both  very  unstable.  On  the  other  hand,  the  combination 
of  iodine  with  oxygen  is  attended  with  an  evolution  of 
heat  of  25,300  calories,  and  an  additional  2600  calories 
are  liberated  when  it  combines  with  water  to  form  iodic 
acid.  Perchloric  acid,  too,  is  formed  with  evolution  of 
heat  (4200  calories),  and  thus  iodic,  periodic,  and  per- 
chloric acid  are  comparatively  stable.  The  heat-change 


146  MODERN   CHEMISTRY 

during  the  formation  of  a  compound,  therefore,  is  connected 
with  its  stability,  although  the  exact  relationship  between 
the  two  is  at  present  unknown. 

Acids  derived  from  Elements  of  Even  Valency. 
— Elements  of  the  molybdenum  and  of  the  sulphur 
groups  can  act  as  dyads,  tetrads,  and  hexads,  and  there  are 
corresponding  compounds  of  chromium,  manganese,  and 
iron,  while  sulphur  and  manganese  are  also  able  to  form 
compounds  analogous  in  formula  to  the  perchlorates,  termed 
the  permanganates  and  persulphates.  Compounds  in 
which  these  elements  function  as  dyads,  however,  have  no 
acid  properties ;  in  the  case  of  chromium,  manganese,  and 
iron,  the  dyad  oxides  have  more  or  less  basic  properties — 
that  is,  their  hydroxides  are  ionised  into  element  and 
hydroxyl — and  they  therefore  form  salts  with  acids.  The 
oxides  MoO2  and  UO2  are  also  feebly  basic  in  character, 
as  well  as  TeO9  ;  but  MnO2  is  the  anhydride  of  a  feeble 
acid,  and  SO2  and  SeO9  form  well-defined  acids,  sulphu- 
rous, H2SO3,  and  selenious,  H2SeOg. 

Oxides  of  Sulphur,  Selenium,  and  Tellurium. 
The  corresponding  Acids. — When  sulphur,  selenium, 
or  tellurium  is  heated  in  air,  the  element  takes  fire  and  burns  ; 
the  chief  product  in  each  case  is  the  dioxide.  That  of 
sulphur  is  a  colourless  gas,  possessing  the  well-known  odour 
of  burning  sulphur  ;  it  is  condensable  to  a  liquid  at  -8°,  and 
it  freezes  at  -79°.  The  gas  is  soluble  in  water,  uniting 
with  it  to  form  the  acid,  H2SO3  ;  on  cooling  the  solution 
to  -6°  and  saturating  it  with  the  gas,  crystals  of  the  formula 
H.^SOg.SH^O  separate;  this  is  a  hydrate  of  sulphurous 
acid.  Selenious  anhydride,  a  white  solid,  also  dissolves  in 
water,  and  from  the  solution  selenious  acid  crystallises 
out,  with  the  formula  H2SeO3.  It  would  naturally  be 
imagined  that  these  acids  should  have  the  structural  formulas 
OS=(OH)2  and  O=Se(OH)2,  inasmuch  as  the  oxides 
are  O=S=O  and  O=Se=O  ;  moreover,  the  chlorides 
O=S=C12  and  O=Se=Cl;,  thionyl  and  selenosyl  chlo- 
rides, are  known ;  and  these  react  at  once  with  water, 


ISOMERIC   SULPHITES  147 

forming  the  acids.  It  is  to  be  presumed  that  there  is  ex- 
change of  chlorine  for  hydroxyl,  as  usual  :  O=S=C1.,  + 
2HOH  =  O=S=(OH)2  +  2HC1.  But  there  is  evi- 
dence, similar  in  kind  to  that  adduced  in  the  case  of  nitrous 
and  phosphorous  acids,  to  show  that  while  sodium  sulphite 
has  the  formula  O=S=(ONa)9,  silver  sulphite  is  better 


expressed  by       /^S\  >  sulphur  being  a  hexad. 

O^     X)Ag 

Isomeric  Sulphites.  —  The  evidence  is  this  :  —  Sul- 

phur alcohol   or   ethyl-hydrosulphide   (also  termed   "  mer- 

captan"),    when    oxidised    by    boiling    with    dilute    nitric 

acid,     is     converted     into     ethyl-sulphonic     acid,     thus  : 

O 

C9H5SH  +  3O  =  C2H-S-OH,     a     monobasic     acid,     of 

li 
O 

O 

I! 
which  the  ethyl  salt  is  C0H5—  S—  O—  C9H5.      Now  sodium 

6 

sulphite,  warmed  with  ethyl  iodide,  yields  an  isomeric  com- 

O 

pound  of  the    formula  C.,H5-O-S-O-C2H5.      This    is 
known,  because  when  saponified  by  boiling  with  alkali,  it  is  con- 

O 

li 
verted  into  alcohol  and  a  suluhite,  thus:  C0H-O—  S—  OC,H, 

/OK 

+  2KOH=2C2H5OH  +  O=S<'  ;    whereas    the    sap- 

XOK 

oniiication    of    ethyl    sulphonate     yields     potassium    ethyl- 

O 

sulphonate     and     alcohol,     thus  :      C2H5—  S—  O—  C2H5  + 

II 
O 


i48  MODERN   CHEMISTRY 

O 

KOH  =  C9H5-S-OK  +  C,H5OH.      And,  moreover,  this 
II 

O 

acid,    when   distilled   with   phosphoric    chloride,   yields   an 
O 
II 

acid    chloride,   C0H5—  S—  Cl,  which  can   be   reduced  with 
II 

O 

nascent  hydrogen  to  ethyl  hydrosulphide,  the  substance  from 
which  the  acid  was  originally  obtained  by  oxidation.  It  is 
therefore  concluded  that  the  carbon  is  directly  united  to  the 
sulphur  atom  in  this  case,  while  in  ethyl  sulphite  the  carbon 
of  the  ethyl  group  is  united  through  oxygen.  It  follows 

/OH 

that  sulphurous  acid   must  have  the  formula   O=S<^        , 

\OH 
Osv      /H 
whereas  sulphonic  acid  should  be  represented  by     ^S\ 

O^    \OH 

The  silver  salt  is  a  sulphonate,  while  the  potassium  salt  is 
a  sulphite.  This  peculiarity  is  not  shown  by  selenium  or 
tellurium.  It  appears  certain  that  they  are  represented  by 


the    formulae    O=Se^  and    O=Te<^  ;    but  it  is 

\OH  \OH 

not  known  which  formula  is  to  be  ascribed  to  a  solution 
of  sulphur  dioxide  in  water. 

Sulphites.  —  The  sulphites,  selenites,  and  telluritesof 
the  alkalies  are  soluble  salts;  those  of  most  of  the  other  metals 
are  sparingly  soluble  in  water.  Double  salts  with  hydrogen 
("  acid  salts  ")  are,  however,  soluble,  e.g.  calcium  hydrogen 
sulphite,  Ca(HSO3)9  ;  and  they  are  all  decomposed  by  the 
stronger  acids,  sulphurous  acid  being  liberated,  if  the  solution 
is  dilute  ;  if  strong,  sulphur  dioxide,  its  anhydride,  comes 
off  in  the  state  of  gas.  Similarly,  selenious  and  tellurous 


ACID   CHLORIDES  149 

acids  are  liberated  on  addition  of  a  strong  acid  to  a  solution 
of  a  selenite  or  tellurite.  Pyro sulphites,  similar  in  kind  to 

o      o 

\(          II 

pyrophosphates,  such  as  KO— S— O— S— OK,  crystallise 
out  on  passing  a  current  of  sulphur  dioxide  through  a 
solution  of  the  carbonate  of  the  alkali. 

Sulphurous  acid  is  a  reducing  agent,  depriving  reducible 
compounds  of  their  oxygen ;  it  itself  is  oxidised  to  sulphuric 
acid  by  the  process.  Owing  to  this  property,  it  is  used  to 
bleach  woollen  goods ;  this  it  does  by  converting  the  in- 
soluble colouring  matter  into  a  soluble  colourless  compound, 
which  can  be  removed  by  washing.  It  is  also  an  antiseptic  ; 
and  sulphites  are  added  to  liquors  undergoing  fermentation, 
when  it  is  desired  to  check  the  action  of  the  ferment. 

Selenious  and  tellurous  acids,  treated  in  boiling  solution 
with  sulphurous  acid,  deposit  selenium  or  tellurium,  thus  : 
H2SeO3.Aq  +  2H2SO3.Aq  =  Se  +  2H,SO4.Aq  +  H2O  ; 
and  with  sulphuretted  hydrogen,  sulphurous  acid  gives  a 
precipitate  of  sulphur  :  H2SO3.Aq  -f-  2H9S.Aq  =38  + 
2H.>O-Aq.  This  brings  to  mind  the  mutual  action  of 
hydrochloric  and  hypochlorous  acids,  and  of  hydriodic  and 
iodic  acids,  where  the  elemens  are  also  liberated. 

Acid  Chlorides.  —  Sulphur  dioxide  combines  with 
chlorine  when  a  mixture  of  the  two  gases  is  exposed  to 
sunlight,  or  when  it  is  passed  over  gently  heated  charcoal. 

CK  Cl 

The  product,  sulphuryl  chloride,      ^>S<;      ,  is  a  colourless 

O^   \C1 

fuming  liquid,  boiling  at  7  7°.     On  adding  it  to  water,  it  imme- 
diately yields  sulphuric  acid  by  replacement  of  the  chlorine 
O.x      7C\     H— OH     O.x      /OH     HC1 
byhydroxyl:     ^S<       +  =     J$/          +          . 

O^  \C1  H— OH  O^  \OH  HC1 
Selenium  and  tellurium  form  similar  compounds ;  and  so 
also  do  molybdenum,  tungsten,  and  uranium,  as  well  as 
chromium.  Molybdyl,  tungstyl,  a-nd  uranyl  chlorides 


150  MODERN   CHEMISTRY 

are  produced  by  passing  chlorine  over  the  dioxides  heated 
to  redness  ;  they  are  not  decomposed  by  water,  but  when 
boiled  with  alkalies  they  are  converted  into  molybdates, 
tungstates,  or  uranates.  Chromyl  chloride,  on  the  other 
hand,  is  formed  by  distilling  together  a  chromate,  a  chloride, 
and  concentrated  sulphuric  acid.  This  amounts  to  the 
action  of  hydrogen  chloride  on  chromium  trioxide,  thus  : 
CrO3  +  2HC1  =  CrO0Cl0  +  H.,O.  The  presence  of  the 
sulphuric  acid  is  necessary  in  order  to  withdraw  and  retain 
water,  for  chromyl  chloride  is  at  once  attacked  by  water, 
chromic  acid  being  formed.  It  is  a  deep  red  fuming  liquid, 
hardly  distinguishable  from  bromine  in  appearance  ;  it  boils 
at  1 1 8°.  A  manganyl  chloride  is  said  also  to  have  been 
prepared. 

The  constitution  of  the  acids  is  inferred  from  that  of  the 
chlorides  ;  and  in  the  case  of  chromium,  an  intermediate 
body  is  known  between  chromyl  chloride  and  potas- 
sium chromate,  termed  chlorochromate  ;  its  formula  is 

O  Cl 

\\      / 
^vCr<(  ;     with     sulphur,    the     corresponding     acid, 

O^       X)K 

chlorosulphuric,  or,  better,  chlorosulphonic  acid  is  known, 

CK          Cl 

/  S<^          .      These  bodies  are  produced  by  the  method  of 

O^    X)H 

mixture;  the  former  by  crystallising  together  anhydro-chro- 
mate  and  chloride  of  potassium:  j^Crr""  ^*/Cr\ 

o^    NOK  KO/   V) 

O^      /OK     O^      /OK 
+  KCI  =     ^Cr/          +      >Cr<  ;  the  latter,  by  the 

O^      \OK     O"     \C1 
union   of  hydrochloric   acid   with   sulphur   trioxide,  thus  : 

°N\  °^        /°H 

J;S  =  O  +  HC1  =  >S<(  .  The  former  consists  of 
O^  O^  \C1 

red  crystals  ;  the  latter  is  a  fuming  liquid,  readily  acted  on 


CHROMATES  151 

by  water,  with  formation  of  sulphuric  and  hydrochloric  acids. 
We  have  thus  with  sulphur  and  with  chromium  the  series  : 

Cl  Osv         OH  O.         OH 


\  \ 

XC1  0<^   \OH 

Cl  O.  OK  O  OK 


o^    NCI'      o^   \ci         o^   NOR 

Chromates.  —  The  starting-point  for  the  chromates  is 
chrome  iron  ore,  Fe(CrO2)2,  a  spinel  (see  p.  100).  It 
is  heated  in  a  powdered  state  with  a  mixture  of  lime  and 
potassium  carbonate,  in  a  reverberatory  furnace,  where  the 
atmosphere  is  a  strongly  oxidising  one.  The  product  is  a 
mixture  of  calcium  and  potassium  chromates  and  ferric 
oxide  :  2Fe(CrO2)2  +  4K2CO3  +  yO  =  Fe2O3  +  4K2CrO4 
4-  4CO2.  The  fritted  mass  is  treated  with  water,  when 
the  chromate  dissolves,  leaving  the  ferric  oxide  insoluble. 
On  evaporation,  potassium  chromate  crystallises  out.  If 
it  is  desired  to  produce  "  bichromate  "  or  anhydrochro- 
mate  of  potassium,  K2Cr2O7,  the  solution  of  the  chromate 
is  treated  with  dilute  sulphuric  acid  ;  calcium  sulphate  is 
precipitated,  and  is  removed  by  settling  ;  on  evaporation, 
sparingly  soluble  sulphate  of  potassium  crystallises  c>ut  ;  and 
after  removal  of  the  crystals,  on  further  evaporation,  "  bi- 
chrome  "  crystallises.  The  conversion  of  the  chromate  into 
the  anhydrochromate  is  represented  by  the  equation  : 
2K2CrO4.  Aq  +  H2SO4.Aq  =  K2Cr2Or.Aq  +  K2SO4.  Aq. 
This  conversion  is  accompanied  by  a  colour-change  ;  for 

the  ions  of  chromate,  CrO4,  are  yellow,  whereas  those  of 

anhydrochromate,  Cr2O7,  are  orange.  On  addition  of 
potassium  hydroxide  to  the  bichromate,  the  opposite  change 
takes  place  ;  the  anhydro-chromate  ion  is  changed  into  the 

+--  +-  +-- 

chromate  ion  :  K2Cr2Or  Aq  +  2KOH.Aq  =  2K2CrO4.Aq 
+  H2O. 


152  MODERN   CHEMISTRY 

Chromic  Acid. — Chromic  acid  is  liberated  on  add- 
ing to  a  concentrated  solution  of  potassium  anhydrochro- 
mate  a  sufficient  excess  of  sulphuric  acid  :  K9Cr2O7.  Aq  + 
H,SO4  =  K2SO4. Aq  +  H2O  +  2CrO3.  The  acid,  in  con- 
centrated solution,  loses  water,  and  deposits  the  trioxide  or 
anhydride  in  crystals  of  a  deep  red  colour.  Chromium 
trioxide  is  a  powerful  oxidising  agent ;  hence  it  may  not  be 
brought  into  contact  with  filter-paper  ;  it  must  be  filtered 
through  a  mat  of  asbestos  or  glass  wool.  The  excess  of 
sulphuric  acid  and  potassium  sulphate  are  washed  out  with 
concentrated  nitric  acid,  in  which  the  anhydride  is  almost 
insoluble  ;  the  nitric  acid  is  then  volatilised  by  gentle  heat. 
This  anhydride  dissolves  in  water,  but  it  is  doubtful  whether 
the  acid  H0CrO4  is  contained  in  the  solution  ;  it  is  more 

+  + 

probable  that  the  ions  are  HH  and  Cr^CX,  from  the  colour, 
and  other  tests,  such  as  the  conductivity. 

Oxidation  by  means  of  a  solution  of  chromic  anhydride 
is  carried  out  either  by  boiling  the  substance  to  be  oxidised 
with  a  mixture  of  bichrome  and  dilute  sulphuric  acid,  or 
with  a  solution  of  chromic  anhydride  in  pure  acetic  acid  ; 

the   chromate   ion,  CrO4   or   Crk>On,  is  changed  into   the 

+  +  +  +     -   - 

chromic     ion     Cr     ;       the     action    is:     K9Cr2O7.Aq  + 

+    -  -  +  +  +  -  -  +    -  - 

4H2SO4.Aq  =  Cr2(SO4)3.Aq  +  K,SO4.Aq  +  4H2O  + 

30.  If  the  sulphuric  acid  is  hot  and  concentrated,  oxygen 
is  evolved  as  gas  ;  if  dilute,  substances  present  in  solution, 
if  they  are  capable  of  being  oxidised,  are  attacked  by  the 
oxygen.  When  chromic  anhydride  is  heated,  it  is  con- 
verted into  chromium  sesquioxide,  Cr9O3,  with  evolution 
of  oxygen. 

Manganates. — Oxides  of  manganese,  if  heated  with 
caustic  alkalies  in  a  current  of  air,  or  with  potassium  or 
sodium  nitrate,  are  converted  into  manganate  ;  the  manga- 
nate,  however,  is  much  more  easily  decomposed  than  the 
chromate,  and,  indeed,  is  stable  only  in  presence  of  excess 


PERMANGANATES  153 

of  alkali.  Manganic  acid  is  incapable  of  existence  ;  an 
attempt  to  liberate  it,  by  addition  of  an  acid  to  its  sodium 
salt,  results  in  the  formation  of  a  permanganate  and  a 
manganous  salt,  thus:  5Na.?MnO4.Aq  + 6H2SO4.Aq  = 
5Na2SO4.Aq  +  MnSO4.Aq  +  4HMnO4.Aq  +  4H2O. 

Permanganates. — While  the  manganates  are  bright 
green,  the  perm?  ^  .nates,  which  are  analogous  to  the  per- 
chlorates,  are  almost  black  ;  they  dissolve  in  water  with  a 
deep  purple  colour  ;  the  best  known  is  the  potassium  salt, 
a  solution  of  which  is  sold  under  the  name  of  "  Condy's 
Fluid."  It  is  also  a  useful  oxidising  agent.  If  an  oxidis- 
able  body  is  boiled  with  its  solution,  it  loses  oxygen,  thus  : 
2KMnO4.Aq  +  3H2O  =  2KOH.Aq  +  2MnO(OH)2 
+  3O  ;  if  an  acid,  such  as  sulphuric  acid,  is  present,  the 
equation  is  :  2KMnO4.Aq  +  3H2SO4.Aq  =  K2SO4. Aq  + 
2MnSO4.Aq  +  50  +  3H2O. 

Ferrates  are  also  known ;  they  are  still  more  unstable 
than  manganates. 

Equations  Simplified. — A  word  may  be  added 
here  with  regard  to  the  somewhat  complicated  equations 
such  as  those  given.  It  is  convenient  to  assume  the  exist- 
ence of  the  anhydride  of  the  acid  as  a  constituent  of  the 
salt ;  thus  potassium  bichromate  may  for  this  purpose  be 
regarded  as  consisting  of  K2O  in  union  with  2CrO3.  On 
acting  on  it  with  sulphuric  acid  in  presence  of  an  oxidisable 
compound,  the  K.,O  may  be  supposed  to  react  with  the  acid 
thus:  K2O+H2SO4  =  K2SO4  +  H2O.  The  chromium 
salt  formed  may  be  regarded  (and  this  was  formerly  the  point 
of  view)  as  a  compound  of  3SOg,  the  anhydride  of  sulphuric 
acid,  with  Cr2O3,  viz.,  Cr2O3.3SO3,  or  Cr2(SO4)3.  The 
formation  of  Cr2O3  from  2CrO8  involves  the  loss  of  30  ; 
hence  the  equation  given  above.  Similarly,  the  oxidising 
action  of  potassium  permanganate  may  be  formulated  thus  : 
K2O.Mn2O7  =  K2O  +  2MnO2  +  30  ;  and  K2O.Mn2O7 
=  K2O  +  2MnO  +  50.  With  water  present  in  the  former 
action,  the  K2O  becomes  KOH,  and  the  manganese  dioxide 
becomes  hydra  ted  ;  with  sulphuric  acid  present  in  the  latter, 


154  MODERN   CHEMISTRY 

the  K2O  is  converted  into  K.,SO4,  and  the  MnO  into 
MnSO4.  This  old  method  of  representing  chemical 
changes  had  much  to  recommend  it  on  the  score  of  simpli- 
city ;  and  it  often  is  found  convenient,  although  it  is  only 
a  partial  expression  of  the  truth. 

Molybdates,  Tungstates,  and  Uranates. — The 
formulas  of  the  molybdates,  tungstates,  and  uranates 
are  analogous  to  those  of  the  chromates ;  for  example, 
K2Mo04,  Na2W04,  (NH4)2UO4.  The  common  ore  of 
molybdenum  is  the  disulphide,  crystalline  scales  resembling 
graphite,  MoSt>,  termed  molybdenite.  On  heating  it  in 
the  air,  or  on  boiling  it  with  concentrated  nitric  acid,  it  is 
oxidised  to  the  trioxide,  MoO3,  a  white  slippery  powder. 
Wolfram,  (Fe,Mn)WO4,  is  the  chief  ore  of  tungsten  ;  on 
boiling  with  concentrated  nitro-hydrochloric  acid,  calcium 
nitrate  and  chloride  go  into  solution,  and  tungstic  acid, 
HoWO4,  remains  as  an  insoluble  yellow  powder.  On 
heating  it,  it  loses  water,  and  yields  the  anhydride,  a 
powder  with  similar  colour,  WO3.  Pitchblende  is  the 
name  of  the  commonest  ore  of  uranium ;  its  formula  is 
UgOg.  On  fusing  it  with  a  mixture  of  nitrate  and  car- 
bonate of  soda,  sodium  uranate  NaQUO4  is  formed  ;  and  on 
adding  acid,  uranic  acid,  H9UO4  is  precipitated,  as  a 
yellow  powder.  On  heating  it  to  300°,  a  scarlet  powder, 
of  the  formula  UO3,  remains.  Ignition  changes  it  into 
U3O8,  possibly  uranium  uranate,  U(UO4)2,  of  the  same 
formula  as  the  natural  mineral.  The  chief  molybdate  is 
that  of  ammonium,  (NH4)9MoO4,  white  crystals  obtained 
by  dissolving  the  acid  in  ammonia  solution  ;  it  is  used  in 
precipitating  phosphoric  acid  as  phospho- molybdate  of 
ammonium,  a  representative  of  many  very  complicated  molyb- 
dates ;  its  formula  is  i6MoO3.P2O5.3(NH4)2O.i4H2O  ; 
it  is  a  derivative  of  one  of  the  condensed  molybdic  acids. 
Sodium  tungstate,  NazWO4,  produced  by  fusing  the  tri- 
oxide with  sodium  carbonate,  is  used  as  a  mordant  in  dye- 
ing, and  it  has  the  property  of  rendering  cotton  and  linen 
fabrics  uninflammable.  The  chief  characteristic  of  uranium 


SULPHUR  TRIOXIDE  155 

trioxide   is   that   of  forming   uranyl   salts,   such   as   uranyl 
nitrate,   (UO0)(NO3)9,  and    acetate,   (UO.,)  (C.,H3O0)0, 
"O 

where  uranyl,  U  =   acts  as  a  dyad  radical.     The  uranates 
il 

O 
are  ill-defined  compounds. 

Sulphur  Trioxide. — The  constitution  of  sulphuryl 
chloride  and  its  conversion  into  sulphuric  acid  has  already 
been  alluded  to.  And  it  may  be  assumed  that  that  of  sulphur 

//Q 

trioxide,  SO3,  is  expressed  by  the  formula  0=8^     >  sulphur 

acting  as  a  hexad.  Although  sulphur  dioxide  unites  directly 
with  chlorine,  it  does  not  combine  with  oxygen,  unless  the 
two  gases  are  brought  intimately  into  contact  by  passing  them 
over  finely  divided  platinum  ;  such  platinum  is  best  prepared 
by  dipping  asbestos  (a  native  magnesium  silicate,  possessing 
a  fibrous  structure)  into  platinic  chloride,  and  subsequent 
ignition,  when  the  chloride  is  decomposed  into  chlorine, 
which  escapes,  and  a  deposit  of  spongy  platinum  on  the 
asbestos.  On  a  large  scale,  sulphur  dioxide,  made  by 
burning  sulphur  or  iron  pyrites,  FeS2,  in  air,  is  concentrated 
by  solution  in  water,  the  gas  being  forced  in  under  some 
pressure  ;  the  solution,  on  being  exposed  to  reduced  pressure, 
gives  up  the  gas,  which  is  thus  freed  from  the  nitrogen  of 
the  atmosphere.  The  sulphur  dioxide  is  then  mixed  with 
air  and  passed  over  the  platinised  asbestos  heated  to  a 
definite  high  temperature.  Combination  ensues,  and  the 
sulphur  trioxide  is  condensed  in  cooled  receivers.  It  is  a 
white,  crystalline,  fuming  substance,  dissolving  in  water 
with  a  hissing  noise  and  with  great  evolution  of  heat.  It 
also  unites  directly  with  hydrogen  chloride,  with  formation 
of  chloro-sulphonic  acid,  Cl— SO0-OH,  a  fuming  very 
corrosive  liquid. 

Sulphuric  Acid. — The  product  on  dissolving  sulphur 
trioxide  in  water  is  sulphuric  acid,  H2SO4 ;  if  smaller 


156  MODERN   CHEMISTRY 

quantities  of  water  be  used  than  are  necessary  for  the 
formation  of  H.2SO4,  various  pyro-  or  anhydro-sulphuric 
acids  are  produced,  the  simplest  of  which  is  the  acid, 
HO— (SO9)— O— (SO2)OH,  analogous  to  some  extent  in  for- 
mula to  pyrophosphoric acid,  ( OH ) 2=PO-O-PO=  ( OH ) 2, 
but  more  closely  resembling  potassium  dichromate.  It, 
too,  is  a  fuming  liquid,  evolving  much  heat  on  addition  of 
water. 

Sulphuric  acid,  however,  is  ordinarily  made  by  bringing 
together  sulphur  dioxide  in  presence  of  steam  with  nitric 
peroxide,  NO2,  and  oxygen.  For  this  purpose,  sulphur 
or  iron  pyrites  is  burned  in  air  ;  the  products  of  combus- 
tion are  passed  through  a  flue  provided  with  a  chamber  in 
which  it  is  possible  to  place,  when  required,  a  pot  containing 
a  mixture  of  sodium  nitrate  and  sulphuric  acid  ;  the  product 
is  nitric  acid,  which  is  at  once  attacked  by  the  sulphur 
dioxide,  yielding  sulphuric  acid  and  nitric  peroxide,  thus : 
2HNO3  +  SO2  =  H2SO4+ 2NO2.  The  gases  next  pass 
up  a  tower,  termed  the  "  Glover  tower,"  after  its  inventor. 
In  this  tower  they  meet  a  spray  of  dilute  sulphuric  acid,  the 
decomposition  product  with  water  of  a  compound  which 
will  afterwards  be  alluded  to,  hydrogen  nitrosyl  sulphate. 
The  hot  gases,  in  contact  with  the  dilute  acid,  evaporate 
much  of  its  water,  which  as  steam  finds  its  way  along  with 
them  up  the  tower.  From  the  Glover  tower  the  gases 
enter  the  first  of  a  series  of  leaden  chambers,  in  which  a 
reaction  occurs  between  the  sulphur  dioxide,  the  nitric 
peroxide,  and  the  steam,  thus :  SO2  +  NO2  +  H2O  =  H2SO4 
+  NO.  Excess  of  air  is  admitted  along  with  the  sulphur 
dioxide,  so  that  there  is  present  in  the  leaden  chamber  a 
considerable  excess  of  oxygen.  By  its  aid,  the  nitric  oxide 
is  re-oxidised  to  peroxide,  which  is  again  attacked  by  the 
sulphur  dioxide,  so  that  the  nitric  oxide  serves  as  a  carrier 
of  oxygen  to  the  sulphur  dioxide.  The  nitrogen  of  the  air 
conveys  the  gases  from  chamber  to  chamber  ;  and  when  it 
has  passed  through  a  sufficient  series  (from  nine  to  thirteen) 
of  chambers,  all  the  sulphur  dioxide  has  been  converted 


SULPHURIC  ACID  157 

into  sulphuric  acid,  and  deposited  on  the  floors  of  the 
chambers,  whence  it  is  run  off  from  time  to  time  ;  it  is 
called  "  chamber-acid."  Formerly,  the  nitric  oxide  and 
peroxide  used  to  escape  into  the  air  and  be  lost,  besides 
causing  a  nuisance  ;  to  save  it,  G-ay-Lussac  devised  a 
means  of  trapping  it  by  passing  the  escaping  gases  up  a 
tower  which  bears  his  name ;  a  stream  of  concentrated 
sulphuric  acid  flows  down  this  tower,  moistening  the  coke 
or  flint  with  which  it  is  filled.  On  coming  into  contact 
with  the  mixture  of  nitric  oxide  and  peroxide,  a  salt  of 
sulphuric  acid  is  formed — hydrogen  nitrosyl  sulphate, 
HO— SO2— O— N=O,  the  group  — N=O  having  replaced 
one  of  the  hydrogen  atoms  of  the  sulphuric  acid.  This 
compound  dissolves  in  the  excess  of  sulphuric  acid  ;  it  is 
conveyed  by  means  of  a  special  pump  to  the  Glover  tower, 
where  it  is  mixed  with  water,  and  is  decomposed,  thus  : 
2HO-SO2-O-NO  +  H2O  =  2HO-SO2-OH  =  NO  + 
NO9.  Although  this  compound  is  formed  by  the  action 
of  concentrated  sulphuric  acid  on  a  mixture  of  NO  and 
NO0,  yet  excess  of  water  causes  the  action  to  proceed  in 
the  opposite  sense ;  this  affords  a  good  example  of  the 
action  of  mass. 

After  the  chamber  acid  has  been  evaporated  in  leaden 
vessels  until  a  portion  of  the  water  is  expelled,  it  is  further 
concentrated  in  vessels  of  platinum,  glass,  or  iron.  The 
dilute  acid  is  without  action  on  lead,  and  the  concentrated 
acid  does  not  attack  platinum  or  iron,  although  iron  is  at 
once  dissolved  by  dilute  acid.  The  heavy  oily  liquid 
remaining  after  evaporation  still  goes  by  its  old  name  of 
"  oil  of  vitrol."  Its  composition  is  not  quite  expressed  by 
the  formula  H2SO4,  however,  for  that  substance  is  unstable, 
and  parts  with  a  trace  of  sulphuric  anhydride  when  heated, 
leaving  a  trace  of  water  in  the  oil  of  vitrol.  It  can  be 
made  by  dissolving  the  right  amount  of  anhydride  in  the 
acid  to  combine  with  that  water ;  the  resulting  acid  melts 
at  10.5°;  oil  of  vitrol  has  a  much  lower  melting-point. 
The  molecular  weight  of  liquid  sulphuric  acid,  determined 


158  MODERN   CHEMISTRY 

by  its  rise  in  a  capillary  tube,  is  very  high,  and  appears  to 
correspond  to  about  3oH9SO4;  on  dilution  it  is  no  doubt 
considerably  lowered,  and  in  dilute  solution  it  is  mostly  in 
the  state  of  ions. 

When  heated  to  about  250°,  sulphuric  acid,  as  oil  of 
vitrol  is  usually  termed,  begins  to  emit  fumes  of  anhydride  ; 
apparent  ebullition  takes  place  at  about  350°,  and  the  acid 
distils  over.  This  is,  however,  really  dissociation  into 
anhydride  and  water  ;  for  the  density  of  the  vapour  is  not,  as 
might  be  expected,  half  the  molecular  weight,  98,  but  only 
24.5,  one  quarter  of  that  number.  And  this  agrees  with 
the  theoretical  density  of  a  mixture  in  equal  proportions  of 
the  vapours  of  the  anhydride  and  water,  for  (40  +  9)  /  2  = 
24.5.  A  considerable  rise  of  temperature  takes  place  on 
mixing  sulphuric  acid  with  water  ;  it  is  not  improbable  that 
the  first  anhydride  of  the  true  ortho-acid  is  formed  ;  the 
compound  of  the  formula  H2SO4.H9O,  which  may  be 
O=S=(OH)4,  melts  at  8°.  The  point  of  maximum 
contraction  of  a  mixture  of  sulphuric  acid  and  water  occurs 
when  the  proportion  corresponds  to  H9SO4.9H2O  ;  this  is 
possibly  S(OH)(J,  but  it  does  not  easily  solidify.  Water 
can  be  withdrawn  from  sulphuric  acid  by  distilling  it  with 
phosphorus  pentoxide,  when  sulphuric  anhydride  is  formed 
and  distils  over. 

Oxidising  Action  of  Sulphuric  Acid. — Sulphuric 
acid  can  behave  as  an  oxidising  agent,  being  itself  reduced. 
This  change  is  produced  when  it  is  heated  with  most  other 
elements.  Thus  with  carbon,  C  +  2H9SO4  =  CO2  +  2 SO., 
+  H,O;  with  sulphur,  S  +  H2SO4  =  3SO2  +  H?O;  with 
copper,  mercury,  iron,  lead,  silver,  &c.,  a  sulphate  is  formed, 
and  sulphur  dioxide  is  liberated  ;  this  may  be  viewed  as  the 
reducing  action  of  hydrogen,  at  the  high  temperature  re- 
quired for  the  reaction,  thus :  Cu  +  H2SO4  =  CuSC>4  +  2H 
and  H2SO4  +  2H  =  2H2O  +  SO2.  The  reduction  goes 
further,  and  some  sulphur  is  liberated,  while  copper  sulphide 
is  formed:  CuSO4  +  8H  =  CuS  +  4H,O  ;  H2SO4 


SELENIC  AND  TELLURIC  ACIDS          159 

Hydriodic,  and  to  a  less  extent  hydrobromic  acid  also, 
are  oxidised  by  sulphuric  acid:  H9SO4  +  2HI  =  I0  + 
2H0O  +  SO2  ;  and  alcohol  and  many  other  compounds  of 
carbon  have  a  reducing  action  on  sulphuric  acid. 

Selenic  Acid. — Selenic  Acid,  H2SeO4,  is  also  a 
colourless  syrupy  liquid ;  it  can  be  produced  by  direct 
oxidation  of  selenium  by  chlorine  water,  but  on  concentra- 
tion the  resulting  hydrochloric  acid  reduces  the  selenic  acid 
to  selenious  acid,  as  hydriodic  acid  reduces  sulphuric  acid. 
It  is  best  prepared  by  addition  of  copper  carbonate  to  the 
mixture  of  selenic  and  hydrochloric  acids  obtained  in  that 
way ;  selenate  and  chloride  of  copper  are  formed ;  the 
mixture  is  evaporated  to  dryness,  and  the  copper  chloride  is 
dissolved  out  with  alcohol,  leaving  the  insoluble  selenate 
behind.  The  selenate  is  dissolved  in  water,  and  on  treat- 
ment with  sulphuretted  hydrogen,  copper  sulphide  is  pre- 
cipitated, and  removed  by  filtration  ;  the  selenic  acid  is 
then  concentrated ;  if  it  contains  a  trace  of  water,  it  is  a 
heavy  liquid ;  but  if  quite  anhydrous,  it  forms  a  solid, 
melting  at  58°. 

Telluric  Acid. — Telluric  acid  is  prepared  from  its 
barium  salt  suspended  in  water,  with  the  requisite  amount 
of  sulphuric  acid ;  the  barium  salt  is  produced  by  heating 
tellurium  with  barium  nitrate.  On  evaporation,  the  hydrate, 
H.)TeO4.2H0O,  deposits  in  white  crystals. 

Sulphate,  Selenates,  and  Tellu rates. — The  sul- 
phates, selenates,  and  tellurates  of  barium  are  nearly 
insoluble  in  water ;  those  of  strontium  and  lead  are  very 
sparingly  soluble,  and  those  of  calcium  are  still  sparingly 
soluble,  though  more  easily  soluble  than  the  salts  previously 
mentioned.  All  these  salts,  therefore,  are  most  conve- 
niently prepared  by  the  addition  of  a  soluble  sulphate, 
selenate,  or  tellurate  to  a  soluble  salt  of  calcium,  stron- 
tium, barium,  or  lead,  thus  :  CaCL.  Aq  +  NaJSO4.  Aq  = 
CaS04.2H20  +  2NaCl.Aq  ;  Pb(NOs)2.Aq  +  K.2SO4Aq 
=  PbSO4  +  2KNO3.Aq.  These  salts  are  still  less  soluble 
in  alcohol  than  in  water,  hence  addition  of  alcohol  to  their 


160  MODERN   CHEMISTRY 

solutions  produces  a  turbidity.  While  barium  sulphate  is 
not  attacked  by  boiling  hydrochloric  acid,  barium  selen- 
ate  evolves  chlorine,  and  is  changed  to  barium  chloride 
and  selenious  acid,  thus  :  BaSeO4  +  4HC1.  Aq  =  BaCl0.  Aq 
+  H2SeO8.  Aq  +  C12  +  H2O. 

All  other  sulphates  are  soluble  in  water,  and  can  there- 
fore be  prepared  by  one  of  the  usual  methods,  such  as 
treatment  of  the  oxide,  carbonate,  or  metal  with  the  acid. 
Dilute  sulphuric  acid  dissolves  magnesium,  zinc,  cadmium, 
aluminium,  chromium,  iron,  manganese,  nickel,  and 
cobalt ;  other  metals  resist  its  attack,  because  their  electro- 
affinity  is  less  than  that  of  hydrogen.  The  order  is :  Cs, 
Rb,  K,  Na,  Li,  Ba,  Sr,  Ca,  Mg,  Al,  Mn,  Zn,  Cd,  Cr, 
Fe,  Co,  Ni,  Pb :— H :  Cu,  Hg,  Ag,  Ft  &c.,  Au.  All 
the  metals  to  the  left  of  hydrogen  in  the  table  are  attacked, 
because  they  receive  their  ionic  charge  from  the  hydrogen 

of  the  dilute  acid:  Zn  +  H?SO4.Aq  =  ZnSO4.Aq  +  H2  ; 
the  zinc  is  ionised,  receiving  its  charge  from  the  hydrogen, 
which  escapes  in  the  molecular  condition.  But  this  trans- 
ference of  charge  appears  to  require  the  contact  of  some 
metal  with  lower  electro-affinity  than  that  of  hydrogen,  for 
pure  zinc  is  not  attacked  by  pure  dilute  acid  ;  in  fact,  the 
arrangement  must  be  analogous  to  that  of  a  battery.  It  is 
possible  that  this  is  due  to  the  protection  of  the  zinc  by  a 
film  of  condensed  hydrogen — in  other  words,  to  polarisa- 
tion ;  contact  with  another  metal  affords  a  means  of  escape 
of  the  charge  from  the  hydrogen,  which  is  evolved,  not 
from  the  surface  of  the  zinc,  but  from  the  surface  of  the 
less  electro-positive  metal. 

With  concentrated  acid,  these  metals,  as  before  remarked, 
are  dissolved  as  sulphates,  with  evolution  of  sulphur  dioxide. 

The  sulphates  form  an  important  group  of  salts.  Among 
the  best  known  are:  Sodium  sulphate,  Na2SO4.ioH2O, 
"  Glauber's  salt,"  contained  in  sea-water  and  in  many 
mineral  springs;  K2SO4,  and  (NH4).,SO4,  hard  rhombic 
prisms  ;  the  double  salts,  NaHSO4,  and  KHSO4,  obtained 


THE  SULPHATES  161 

by  mixture  ;  when  heated,  these  salts  lose  water  and  are 
converted  into  pyrosulphates  :  2  KHSO4  =  H9O  -f-  K2S9O7. 
CaSO4  occurs  native,  as  anhydrite,  and  CaSO4.2H2(3,  as 
gypsum  and  alabaster.  Gypsum,  when  gently  heated, 
loses  its  water,  and  is  then  known  as  "  plaster  of  Paris  ;  " 
on  mixing  it  to  a  paste  with  water,  combination  takes  place 
slowly,  and  the  plaster  "  sets  ;  "  and  in  this  way  casts  may 
be  taken.  SrSO4  is  found  native  as  celestine  ;  BaSO4,  as 
heavy-spar  or  barytes.  It  is  the  commonest  mineral 
containing  barium  ;  from  it  barium  salts  are  prepared,  by 
heating  it  with  ground  coke,  which  reduces  it  to  the  sul- 
phide :  BaSO4  +  40  =  ^.CO  +  BaS.  The  barium  sulphide 
is  then  dissolved  in  the  appropriate  acid,  and  the  required 
salt  is  made.  Precipitated  barium  sulphate  is  known  as 
"  permanent  white  ;  "  owing  to  its  low  price,  it  is  much 
used  as  a  paint,  although  its  covering  power  is  small. 

MgSO4.7H2O,  ZnSO4.7H2O,  and  CdSO4.yH2O,  as 
well  as  FeSO4.7H2O,  MnSOjyl-^O,  and  the  correspond- 
ing cobalt  and  nickel  salts,  are  "  isomorphous,"  that  is,  they 
crystallise  in  the  same  form — rhombic  prisms.  Magnesium 
sulphate,  or  "  Epsom  salts/'  is  present  in  sea-water  and 
in  many  mineral  waters ;  it  also  occurs  in  the  salt  deposits 
at  Stassfurth,  in  S.  Germany,  and  is  termed  kieserite.  It 
is  used  as  a  purgative.  Zinc  sulphate  is  known  as  "  white 
vitriol,"  and  ferrous  sulphate  as  "green  vitriol"  or 
"copperas."  A  large  number  of  double  salts  exists,  of  the 
formulas  of  which  MgSO4.K0SO4.6H2O  may  serve  as  a 
type  ;  they  are  all  soluble,  and  they  are  ionised  in  solution 
into  the  same  ions  as  the  simple  salts  would  furnish  ;  thus, 

+  +      + 

the  ions  of  the  salt  mentioned  above  are  Mg,  2K,  and  2SO4. 
They  differ  in  this  respect  from  such  salts  as  K2SiF6,  of 

+ 

which  the  ions  are  2K  and  SiF6.  The  alums  form  a 
similar  series  of  double  salts,  in  which  monad  metals,  such 
as  sodium,  potassium,  and  ammonium,  and  triad  metals, 
aluminium,  chromium,  iron,  manganese  and  others,  are 
combined  together  as  sulphates  with  water  of  crystallisa- 

VOL.   II.  L 


i62  MODERN   CHEMISTRY 

tion:  K2SO4.Al2(SO4)3.24H,O,orKAl(SO4),.i2H.2O. 
The  molecular  weight  of  the  compound  is  unknown  ;  hence, 
as  usual,  the  simpler  formula  is  preferable.  These  com- 
pounds are  named  from  their  analogy  with  the  original 
"  alum,"  of  which  the  formula  is  given  above  ;  they  all 
crystallise  in  regular  octahedra,  and,  like  all  true  isomor- 
phous  salts,  they  are  able  to  crystallise  together  ;  so  that  if 
a  crystal  of  KA1(SO4).,. I2H.,O  is  placed,  for  example, 
in  a  solution  of  (NH4)2Cr(SO4)2.i2H2O,  the  latter  will 
form  a  dark-red  layer  on  the  surface  of  the  former. 
"  Alum "  finds  use  as  a  mordant;  when  textile  fabrics 
are  boiled  in  its  solution,  the  fibre  becomes  incrusted  with 
a  layer  of  aluminium  hydroxide,  and  when  subsequently 
dyed  the  colouring  matter  is  retained  in  combination  with 
the  alumina  and  with  the  fibre,  so  that  it  cannot  be  removed 
by  washing.  This  phenomenon  depends  on  the  fact  that 
aluminium  sulphate  is  partially  hydrolysed  by  water  into 
A1(OH)3  and  3H2SO4;  the  adhesion  of  the  alumina  to 
the  fibre  is  attributed  to  "  adsorption,"  a  term  applied  to 
the  adhesion  of  gases,  liquids,  or  of  substances  in  solution, 
to  the  surface  of  solids.  A  solution  of  alum  also  gives 
coloured  precipitates  with  many  dye-stuffs,  which  are 
known  as  "  lakes."  Selenic  acid  also  yields  alums. 

Bismuth  sulphate,  Bi2(SO4)3,  obtained  by  evaporating 
a  solution  of  bismuth  oxide,  Bi2Og,  in  sulphuric  acid,  forms 
acicular  crystals,  which,  on  addition  of  water,  like  all  other- 
bismuth  salts,  yield  a  basic  salt,  in  which  the  group  O=Bi-, 
bismuthyl,  plays  the  part  of  a  monad  metal ;  hence  the 
formula  of  the  basic  sulphate  is  (O=Bi)9SO4  ;  it  is  an 
insoluble  powder.  Copper  sulphate,  or  "  blue  vitriol," 
CuSO4.5H2O,  forms  blue  soluble  crystals;  silver,  mer- 
curous,  and  mercuric  sulphates,  Ag2SO4,  Hg2SO4,  and 
HgSO4,  are  sparingly  soluble,  white  crystalline  powders. 

As   the   ion   SO4  is  colourless,  all  these  salts  possess  the 

-¥  + 

colour   of  the  metallic   ion  which  they  contain  ;   thus,  Fe 


SALTS   OF   RADICALS  163 


+  4-  +  +  +  +  +  +  ++  +  + 

is  green,  Mn  pink,  Cr   green,   Fe  yellow,  Ni   green,  Co 

red,  Cu  blue,  and  the  others  colourless. 

Sulphates  of  the  alkali-  and  alkaline-earth  metals  are 
stable  at  all  temperatures  lower  than  that  of  the  electric  arc  ; 
but  all  other  sulphates  decompose,  the  primary  product  being 
the  oxide  of  the  metal  and  sulphuric  anhydride  ;  the  latter, 
however,  being  unstable  at  a  red-heat,  decomposes  partly 
into  sulphur  dioxide  and  free  oxygen.  This  decomposition 
is  made  use  of  in  the  preparation  of  "  Nordhausen  sulphu- 
ric acid,"  a  fuming  liquid,  consisting  chiefly  of  H9S9O7  ; 
it  is  made  by  distilling  partially  dried  ferrous  sulphate  from 
fireclay  retorts:  2FeSO4=  Fe9O3  +  SO2  +  SO3  ;  the 
pyrosulphuric  acid  is  produced  by  the  union  of  the  anhy- 
dride with  water:  2SO3  -f-  H2O  =  H9  S9Or  The  iron 
oxide  has  a  fine  red  colour,  and  is  sold  as  a  paint  under  the 
name  "  Venetian  red." 

Salts  of  Alkyl  Radicals. — Salts  of  the  alkyl  radi- 
cals are  as  a  rule  volatile  ;  they  are  produced  by  distilling 
the  alcohols  with  the  respective  acid.  Ethyl  nitrite,  for 
example,  is  formed  by  distilling  a  mixture  of  alcohol, 
sodium  nitrite,  and  sulphuric  acid  :  NaNO9  +  H9SO4.  Aq  -h 
C9HrOH  =  C,HrNO0  +  NaHSO4.Aq.  "  It  is  a  volatile 

2       5  -       5  -•  4         T. 

liquid,  with  a  pleasant  odour,  which,  when  boiled  with 
potash,  is  hydrolysed,  with  formation  of  sodium  nitrite  and 
ethyl  alcohol :  C9H5NO2  +  KOH.Aq  =  K-O-N=O.Aq 
+  C2H5OH.  The  nitrate,  C,H5ONO2,  cannot  be  pre- 
pared from  nitric  acid  and  alcohol  unless  the  presence 
of  nitric  peroxide  is  excluded  ;  for  this  purpose  urea, 
CO(NH9)2,  is  added  in  small  proportion  to  the  mixture  ;  its 
presence  prevents  the  oxidation  of  the  alcohol,  and  brings 
about  the  normal  action  C2H5OH  +  HNO3  =  C2H&NO3 -f- 
H9O.  The  nitrate  resembles  the  nitrite  in  properties.  On 
mixing  alcohol  with  sulphuric  acid  there  is  a  considerable  rise 
in  temperature,  and  hydrogen  ethyl  sulphate  is  produced  : 
C2H5O  H  +  HO-SO2-OH  =  HO-SO2-OC  9H5  +  H2O. 
A  considerable  excess  of  sulphuric  acid  must  be  present  in 


164  MODERN   CHEMISTRY 

order  to  ensure  the  nearly  complete  conversion  of  the 
alcohol  into  the  ethyl  salt.  To  remove  this  excess,  calcium 
carbonate  is  added,  which  forms  sulphate  of  calcium  and 
a  double  sulphate  of  ethyl  and  calcium,  Ca(C9H5SO4)2  ; 
the  former  is  nearly  insoluble  in  water,  while  the  latter  is 
readily  soluble  ;  from  the  calcium  salt  the  acid  may  be  pro- 
duced by  addition  of  the  theoretical  amount  of  sulphuric 
acid.  On  evaporation  it  is  a  syrupy  liquid  ;  it  decomposes 
when  heated  into  ethylene,  sulphur  dioxide,  carbon  mon- 
oxide, and  carbon  dioxide.  As  seen  by  the  formula  of  the 
calcium  salt,  the  acid  is  a  monobasic  one.  The  potassium 
salt,  for  example,  has  the  formula  K(C^H5)SO4 ;  the  salts 
are  all  soluble.  Similar  acids  are  formed  from  other  alkyl 
radicals,  such  as  methyl,  amyl,  &c. 

ThlOSltlphates. — Some  other  acids  of  sulphur  remain 
to  be  noticed.  Among  these  is  thiosulplmric  acid, 
H2S2O3,  of  which  the  sodium  salt  is  produced  by  digesting 
together  sodium  sulphite  with  sulphur,  just  as,  with  oxygen, 
sodium  sulphate  is  formed.  In  the  latter  case  it  may  be 
supposed  that  the  atom  of  oxygen  inserts  itself  between  the 
sodium  atom  and  the  sulphur  atom  with  which  it  is  in  com- 

o  o 

li  i: 

bination,   thus :    Na-Q-S-Na  +  O  =  Na-Q-S-Q-Na  ; 

I!  li 

O  O 

o  o 

I.  ii 

Na-O-S-Na  +  S  =  Na-O-S-S-Na  ;     hence    the    name 

I  I1 

O  O 

"  thio  "  sulphate,  the  "  thion,"  or  sulphur,  replacing  the 
oxygen  of  sulphuric  acid.  The  sodium  salt  forms  large 
transparent  crystals  of  the  formula  Na2S2O3.5HQO  ;  the 
barium  salt  is  sparingly  soluble,  and  forms  a  crystalline 
precipitate  on  adding  a  solution  of  the  sodium  salt  to  one  of 
barium  chloride  ;  the  lead  salt  is  insoluble,  and  the  silver 
salt  is  a  white  precipitate,  which  rapidly  turns  dark  on 


IODOMETRY  165 

application  of  heat,  being  converted  into  silver  sulphide  : 
Ag2S2O3  +  H2O.Aq-Ag,S  +  H2SO4.Aq.  On  acidify- 
ing any  one  of  the  soluble  salts,  the  acid  is  momentarily 
liberated  ;  but  it  immediately  decomposes  into  sulphurous 
acid  and  sulphur,  H9S2O3.Aq  =  H0SOg.Aq  + S,  the  latter 
rendering  the  liquid  milky.  The  sodium  salt,  when  a  solu- 
tion of  iodine  in  one  of  potassium  iodide  is  added  to  it, 
undergoes  the  reaction  :  2Na0S.7O3.  Aq  +  I0. Aq  =  zNal. Aq 
+  Na9S4O6. Aq.  The  salt  formed  is  named  tetrathionate 
of  sodium.  It  will  be  considered  shortly. 

lodometry. — A  solution  of  sodium  thiosulphate  con- 
taining 248  grams,  made  up  to  a  litre  with  water,  reacts 
quantitatively  with  one  containing  127  grams  of  iodine  per 
litre  ;  the  colour  of  the  iodine  disappears,  and  the  vanishing 
of  the  last  trace  of  iodine  can  be  ascertained  by  the  addition 
of  some  starch  paste,  which  gives  a  blue  colour  so  long  as 
any  free  iodine  remains  unconverted  into  ions  ;  such  a  solu- 
tion is  commonly  used  in  estimating  iodine,  or  in  determin- 
ing the  quantity  present  in  solution  of  any  substance  which 
has  the  property  of  liberating  iodine  from  acidified  iodide, 
i.e.  from  hydriodic  acid,  such  as  free  chlorine,  a  hypo- 
chlorite,  or,  indeed,  any  oxidising  agent. 

On  boiling  together  solutions  of  sodium  thiosulphate  with 
ethyl  iodide,  sodium  ethyl  thiosulphate  is  formed  ;  its 
O 
ii 
formula    is    Na~ O~ S~ S~C9H5,    for,    when    mixed    with 

6 

barium  chloride,  the  barium  salt,  which  is  unstable,  decom- 
poses into   barium   dithionate   and  ethyl   disulphide,   thus  : 
X)-SO.-S(C0H5)  /O-SO0          S(C,H.) 

Ba<  =    B<         I     ^    +     I 

M>-SO2-S(C2H5)  X)-SO2          S(C2H5) 

This    decomposition    renders    two    suppositions    probable  : 

CK          SH 

that    thio-sulphuric    acid    has    the    formula         /S\  » 

\OH 


166  MODERN   CHEMISTRY 


, 
and  not        ^^\  >  ar>d  tnat  dithionic  acid  is  constitu- 

O^    \OH 

O2S-OH 

tionally  represented  by        I 

O2S-OH 

Hydrosulphites.  —  Hydrosulphurous  acid,  H2S2O4, 
sometimes  called  "  hyposulphurous  acid,"  is  produced 
as  zinc  salt  by  the  action  of  metallic  zinc  on  sulphurous 
acid.  The  liquid  turns  brown,  and  possesses  great  reducing 
power.  The  sodium  salt,  which  is  better  known,  is  pro- 
duced by  digesting  zinc  turnings  with  a  concentrated  solu- 
tion of  hydrogen  sodium  sulphite  :  Zn  +  4HNaSO3.  Aq  = 
Na2Zn(SO3)2  +  Na2S2O4.Aq  +  2H2O  ;  the  sodium  zinc 
sulphite  crystallises  out  on  addition  of  alcohol,  leaving  the 
hydrosulphite  in  solution.  On  cooling  the  solution,  slen- 
der crystals  of  the  hydrosulphite  separate.  The  solution 
absorbs  free  oxygen  so  rapidly  that  it  turns  warm  ;  it  is 
used  as  a  reducing  agent  in  indigo-dyeing  ;  indigo-blue  is 
converted  by  the  hydrogen  of  water  (of  which  the  oxygen 
enters  into  combination  with  the  hydrosulphite,  convert- 
ing it  into  sulphite)  into  a  colourless  substance,  termed 
indigo-white  ;  this  body  being  soluble,  penetrates  the  fibre 
of  fabrics  dipped  into  the  solution,  and  on  exposure  to  air, 
indigo-blue,  with  its  usual  colour,  is  deposited  as  an  in- 
soluble precipitate  in  the  cloth.  By  help  of  sodium  hydro- 
sulphite,  too,  a  ferrous  salt  may  be  deprived  of  ferric  so 
completely  that  it  gives  a  nearly  white  precipitate  with 
alkalies  ;  the  usual  colour  of  the  impure  ferrous  hydroxide 
is  a  dirty  green. 

Thionates*  —  Manganese  dithionate  is  produced  by 
passing  a  current  of  sulphur  dioxide  through  freshly  pre- 
pared manganese  dioxide  suspended  in  water,  made  by 
boiling  potassium  permanganate  with  alcohol.  The  equa- 
tion MnO2.nH2O  +  2SO2.Aq  =  MnS2O6.Aq  represents  the 
change.  On  addition  of  barium  hydroxide  to  the  man- 
ganese salt,  manganous  hydroxide  is  thrown  down,  and 


THIONATES  167 

barium  dithionate  is  left  in  solution.  From  it,  the  acid 
may  be  prepared  by  the  addition  of  the  requisite  amount  of 
sulphuric  acid ;  and  the  other  salts,  by  addition  of  the 
appropriate  sulphate.  The  acid,  concentrated  by  evapora- 
tion at  a  low  temperature,  is  a  sour,  syrupy  liquid  ;  when 
heated,  it  decomposes  into  sulphur  dioxide  and  sulphuric 
acid. 

Trithionic  acid,  H2S3O6,  is  also  known ;  it  is  a  still 
more  unstable  liquid. 

Tetrathionate  of  sodium,  as  already  remarked,  is  pro- 
duced by  addition  of  a  solution  of  iodine  to  a  thiosulphate  ; 
it  is  precipitated  on  addition  of  alcohol.  The  acid  forms 
a  colourless  solution,  with  strong  acid  taste.  The 
method  of  its  formation  gives  a  clue  to  its  constitution  : 
NaO-S(O9)-S-Na  I  Nal  NaO-S(O2)-S 

+   I    =          +  I  • 

NaO-S(02)-S-Na      I        Nal     NaO-S(O2)-S 

Pentathionic  acid,  H9S5O6,  is  produced  by  passing  a 
current  of  hydrogen  sulphide  through  a  dilute  solution  of  sul- 
phurous acid,  along  with  tri-  and  tetrathionic  acids  :  5Ht>8 
+  5SO2.Aq.  =  H2S5O6.Aq  +  4H2O  +  58  is  the  equation 
usually  given.  Excess  of  hydrogen  sulphide,  passed  for  a 
long  time,  results  in  the  reaction  2H9S  +  SO9.Aq  = 
2H2O.Aq  +  3S.  The  tri-,  tetra-,  and  pentathionates, 
when  heated,  yield  a  sulphate,  sulphur  dioxide,  and  free 
sulphur. 

Highly  Oxidised  Acids- — Of  recent  years,  a  con- 
siderable number  of  salts  of  acids  more  highly  oxidised 
than  any  of  those  already  mentioned  has  been  prepared.  It 
has  long  been  known  that  on  addition  of  hydrogen  dioxide 
to  a  solution  of  potassium  bichromate  acidified  with 
sulphuric  acid,  a  bright  blue  colour  is  produced,  and  that 
this  coloured  substance  can  be  extracted  by  ether  from  its 
aqueous  solution.  The  compound  has  recently  been 
identified  as  perchromic  acid,  CrO4(OH);  for,  on 
adding  to  the  cooled  blue  solution  a  solution  of  ammonia 
in  ether,  a  violet  precipitate  of  CrO4(O— NH4).H0O0  is 


168  MODERN   CHEMISTRY 

thrown  down ;  and  if  an  etherial  solution  of  potassium 
hydroxide  be  added,  the  potassium  salt  of  similar  formula 
is  precipitated.  These  bodies  are  explosive. 

Persulphates  of  potassium  and  ammonium  are  produced 
by  passing  a  current  of  electricity  through  concentrated 
solutions  of  the  sulphates  in  water.  The  persulphate  is 
sparingly  soluble,  and  deposits  in  white  crystals.  The 
formula  appears  to  be  M,,S0O8  (M  =  monad  metal). 
The  acid  has  bleaching  powers,  and  gradually  decomposes 
into  sulphuric  acid  and  ozone. 

Perborate  of  sodium,  NaBO3,4H0O,  is  similarly  pre- 
pared, or  it  may  be  produced  by  cooling  a  solution  of 
borax  to  which  some  caustic  soda  and  hydrogen  peroxide 
have  been  added.  It,  too,  is  a  sparingly  soluble  salt,  pos- 
sessing bleaching  properties. 

Percarbonate  of  sodium,  Na0CO4.  iiH0O,  is  similarly 
prepared  by  addition  of  alcohol  to  a  solution  of  sodium 
carbonate,  to  which  a  solution  of  hydrogen  peroxide  has 
been  added.  It  is  a  white,  extremely  unstable  compound, 
possessing,  like  the  other  similar  salts,  great  oxidising 
power. 


CHAPTER   IX 

The  Nitrides  and  Phosphides,  Arsenides  and 
Antimonides  —  Complex  Amines  and  their 
Salts  —  Acid  Amides  —  The  Cyanides  and  the 
Double  Cyanides. 

Analogy  between  Oxides  and  Nitrides.  —  Nitro- 

gen and  phosphorus  are  best  characterised  by  the  compounds 
in  which  they  act  as  triads.  For  just  as  an  oxide  or 
hydroxide  may,  as  was  customary  during  the  era  of  the 
theory  of  "  types,"  be  regarded  as  water  in  which  the 
atoms  of  hydrogen  are  more  or  less  completely  replaced  by 
atoms  of  a  metal  ;  so  from  analogy  it  is  to  be  inferred  that 
compounds  should  be  preparable  which  should  be  similarly 
related  to  ammonia  and  to  hydrogen  phosphide.  The 
following  graphic  formulae  will  render  the  conception 
clear  :  — 

H-O-H          ->          Na-O-H          -+        Na-O-Na  ; 
H-NH2  ->          Na-NH2  ->         Na-N=Na2  ; 

H-O-H  )  0-H 

> 


>       -          Ca 
H-O-H  )  0-H 

H-NH2  )  ,NH2  , 


H-NH0  )  \NH2 

169 


170  MODERN   CHEMISTRY 


H-O-H)  /OH  XO 

H-O-H  I    ->  Cr^  OH      ->     Cr^          -> 
H-O-H  XOH  \OH  Cr/ 


H-NH0  )  /NH0  /NH 

H-NH:  y  ->  c<  NH;  ->    c^        ->  CI=N. 

H-NH"  )  NtfHg  \NH2 

But  although  most  elements  combine  with  oxygen  directly, 
there  are  only  a  few  which  burn  in  nitrogen.  Among  these 
are  lithium,  calcium,  and  magnesium  ;  boron  and  titanium 
also  possess  this  property.  The  nitrides  of  the  other 
elements  are  practically  unknown.  These  nitrides  are 
attacked  by  water  ;  the  three  first  with  violence  at  the 
ordinary  temperature  ;  the  two  last,  when  heated  in  a 
current  of  steam.  The  products  are  the  hydroxide  of  the 
metal  and  ammonia  ;  or  with  boron  and  titanium,  owing  to 
the  high  temperature  of  action,  the  oxide,  thus  :  Mg3N2 
+  3H2O.Aq=  3Mg(OH)2  +  2NHrAq. 

Nitrides.  —  Lithium  nitride,  LigN,  is  a  dark-coloured 
substance  ;  it  is  formed  at  the  ordinary  temperature  on  expos- 
ing metallic  lithium  to  the  air.  Calcium  nitride,  Ca.N9,  is  a 
greyish-yellow  substance  ;  and  magnesium  nitride,  Mg3N2, 
a  yellow  powder.  Combination  takes  place  readily  with 
great  evolution  of  heat  when  a  mixture  of  dry  lime  with 
magnesium  powder  is  heated  to  dull  redness  in  a  current  of 
nitrogen  ;  this  affords  a  convenient  method  of  separating 
nitrogen  from  the  indifferent  gases  of  the  atmosphere,  and 
preparing  the  latter  in  a  state  of  purity.  Boron  nitride, 
BN,  is  a  white  amorphous  powder  ;  it  can  also  be  produced 
by  heating  to  redness  a  mixture  of  boron  oxide  with  ammo- 
nium chloride,  until  excess  of  the  chloride  has  volatilised. 

Hydrazoates.  —  Besides  these  compounds,  which  may 
be  regarded  as  the  analogues  of  the  oxides,  a  series  of 
nitrides  is  known,  which  correspond  in  formula  with 
hydrazoic  acid,  HN3.  The  starting-point  for  these  com- 
pounds is  sodamine,  NaNH2  (see  below).  This  compound 


HYDRAZOATES  171 

is  heated  to  300°  in  a  series  of  small  flasks  in  a  current  of 
nitrous  oxide,  when  the  following  reaction  takes  place : 
2NaNH2  +  N2O  =  NaN3  +  NaOH  +  NH3.  The  change 
which  takes  place  is  more  obvious  when  the  reaction  is  con- 

/N        /N 

ceived  to  occur  in  two  stages:  NaNH0  +  O<    II  =  NaN/ 

\N  \N 

+  H2O;  and  NaNH,  +  H2O  =  NaOH  +  NH3.  The 
product  of  the  reaction  is  dissolved  in  water,  acidified  with 
dilute  sulphuric  acid,  and  distilled  :  NaNg.Aq  +  H0SO4.  Aq 
=  HN3.Aq  +  NaHSO4.  Aq.  The  distillate,  which  is  a 
dilute  solution  of  hydrazoic  acid,  has  a  peculiar  odour,  and 
if  its  vapour  be  inhaled,  fainting  may  result ;  it  is  necessary 
to  take  precautions  to  distil  it  in  a  good  draught.  The 
solution  has  an  acid  reaction ;  salts  may  be  prepared  by 
neutralisation  with  the  hydroxides  or  carbonates  of  the 
metals.  The  ions,  -N3,  are  colourless,  and  the  salts  of 
colourless  ions  are  themselves  white.  Those  of  lithium, 
sodium,  potassium,  magnesium,  calcium,  strontium, 
barium,  and  zinc  are  crystalline  ;  their  formulae  are  M'N3 
and  M//(N3)2  respectively.  Silver  hydrazoate,  AgN3, 
closely  resembles  the  chloride  in  appearance  and  in  in- 
solubility ;  it  is,  however,  dangerously  easy  to  explode, 
and  should  be  prepared  dry  only  in  minute  quantity,  and 
treated  with  the  utmost  precaution.  Titration  with  a 
deci-normal  solution  of  silver  nitrate  affords  a  convenient 
method  of  determining  the  strength  of  a  solution  of 
hydrazoic  acid,  or  of  analysing  the  hydrazoates  ;  it  is  easy 
to  recognise  the  point  when  all  hydrazoic  acid  has  been 
removed  as  the  insoluble  silver  salt. 

Amines. — Substituted  ammonia,  in  which  one  atom  of 
hydrogen  is  replaced  by  an  element,  is  the  analogue  of  the 
hydroxides.  Such  bodies  are  termed  amines  or  amides. 
Sodamine,  NaNH2,  is  easily  prepared  by  passing  a  current 
of  ammonia,  dried  by  passing  it  through  a  tower  filled  with 
soda-lime,  through  an  iron  U-tube  containing  sodium,  and 
heated  to  about  300°.  The  gas  is  rapidly  absorbed,  while 


172  MODERN   CHEMISTRY 

hydrogen  is  evolved  :  2NH3  +  2Na  =  2NaNH0  +  H2. 
When  the  sodium  has  been  all  converted  into  sodamine, 
the  tube  is  emptied  by  pouring  out  its  contents.  Sodamine 
is  a  white  brittle  substance,  with  crystalline  fracture,  not 
unlike  caustic  soda,  melting  at  about  100°.  So  long  as  it  is 
kept  dry  it  is  quite  permanent,  but  with  moisture  it  at  once 
reacts,  forming  ammonia  and  caustic  soda  :  NaNH..,  +  HOH 
=  NaOH  +  NH3.  Similar  compounds  can  be  made  with 
lithium,  potassium,  rubidium,  and  probably  caesium. 
The  corresponding  compound  of  zinc,  Zn(NH0)9,  is  a 
white  powder,  insoluble  in  ether,  formed  along  with  ethane 
or  methane  by  the  action  of  ammonia  on  zinc  methide  or 
ethide  :  Zn(CH8)2  +  2NH3  =  Zn(NH2)2  +  2CH4. 

Guanidine. — An  attempt  to  produce  the  amine  of 
carbon,  C(NH2)4,  by  the  action  of  ammonia  on  such 
a  body  as  carbon  tetrachloride  or  ethyl  orthoformate, 
C(OC9Hr)4,  according  to  the  equations  CCl4  +  4NHg 
=  C(NH2j  +4HC1,  or  C(OC2H5)4  +  4NH3  =  C(NH2)4 
+  4HOC9H5,  fails,  owing  to  loss  of  ammonia.  For  just 
as  orthocarbonic  acid,  C(OH)4,  loses  water,  yielding 
ordinary  carbonic  acid,  so  carbon  tetramine  loses  ammonia  ; 
the  product  is  named  guanidine,  and  has  the  formula 
HN  =  C(NH2)2;  its  analogy  with  O  =  C(OH)2is  easily 
seen.  Guanidine  is  a  white  crystalline  substance,  which, 
like  ammonia,  unites  with  acids  to  form  salts. 

On  comparing  the  formulas  of  carbonic  acid  and  guani- 
dine, it  is  evident  that  several  intermediate  compounds 
should  be  capable  of  existence.  The  series  is  : — 

NH2 
0  =  C(OH)0  HN  =  C(OH)0  0  =  C< 

X)H 
(0  (2)  (3) 

/OH 

O  =  C(NH9)2         HN  =  C<  HN  =  C(NH0).7. 

XNH0 
(4)  15)  (6) 


CARBAMATES  173 

Of  these,  the  best  known  are  the  ammonium  salt  of  (3), 
which  is  termed  carbamic  acid,  and  (4),  the  important 
compound  urea  or  carbamide. 

Carbamates.  —  Ammonium  carbamate,  known  by 
the  familiar  name  of  "  smelling  salts/'  is  formed  by  mixing 
ammonia  and  carbon  dioxide  gases  :  CO9  +  2NHg  = 
H2N  -  CO  -  ONH4.  It  is  a  white  crystalline  compound, 
soluble  in  water  and  smelling  of  ammonia.  Its  solution, 
when  fresh,  contains  the  compound  of  which  the  formula 
is  given  above  ;  but  after  standing,  it  is  converted  by 
absorption  of  water  into  ammonium  carbonate.  This  has 
been  ascertained  by  treating  the  freshly  prepared  solution 
with  sodium  hypochlorite,  when  only  half  the  nitrogen 
which  the  substance  contains  is  evolved  : 


2H0N-CO-ONH4.  Aq  +  sNaOCl.  Aq  = 
2H2N-CO-OH.Aq  +  3H20  +  3NaCl  +  N2  ; 

on  the  other  hand,  with  a  hypobromite,  all   the  nitrogen 
is  evolved  : 

H0N-CO-ONH4.Aq  +  3NaOBr.  Aq  =  CO2  + 


Now,  ammonium  salts  yield  up  their  nitrogen  when 
mixed  with  a  solution  of  a  hypochlorite  ;  hence  it  is  con- 
cluded that  the  compound  contained  in  a  fresh  solution 
is  ammonium  carbamate.  But  on  standing,  the  solution 
changes,  and  after  some  time  it  yields  all  its  nitrogen 
on  treatment  with  hypochlorite  ;  hence  the  assumption  of 
the  elements  of  water  and  a  change  into  ammonium  car- 
bonate may  be  inferred:  H2N-CO-ONH4.Aq  +  H,O  - 
H4N—  O—  CO—  ONH4.  Aq.  But  ammonium  carbamate  may 
conceivably  possess  the  formula  HO—  C(NH)—  ONH4  ; 
and  it  may  be  that  it  is  the  =NH  group  which  resists 
attack.  This  last  supposition  is  confirmed  by  the  behaviour 
of  urea  with  hypochlorite  ;  for  with  it,  too,  only  half  the 
nitrogen  is  evolved. 

Carbamide.  —  Urea  or  carbamide,  to  which  the  for- 


174  MODERN   CHEMISTRY 

mula  O  =  C(NH>>)>2  is  generally  ascribed,  is  the  form  in 
which  by  far  the  largest  part  of  the  nitrogen  is  evolved 
which  is  consumed  as  food  by  animals.  It  may  be  directly 
prepared  from  urine  by  evaporation  to  one-third  of  its  bulk, 
and  addition  of  nitric  or  of  oxalic  acid ;  the  sparingly 
soluble  nitrate  or  oxalate  is  precipitated;  the  salt  is  purified 
by  recrystallisation  from  water,  and  is  then  mixed  with 
caustic  soda  and  evaporated  to  dryness.  On  treatment 
with  alcohol,  the  urea  alone  dissolves,  and  deposits  in 
crystals  from  a  concentrated  solution.  It  is  a  white,  easily 
soluble  substance,  with  a  saline  taste.  It  unites  with  acids, 
forming  salts  ;  but  as  the  carbonyl  group,  CO,  has  the 
property  of  conferring  acidity  on  neighbouring  atoms  of 
hydrogen,  the  basic  qualities  of  only  one  of  the  two 
amido-groups,  — NH2,  can  display  itself;  hence  the  for- 
mula of  the  hydrochloride  is  CO(NH2)2.HC1,  and  not 
CO(NH2)2.2HC1,  as  might  be  expected.  It  is  therefore 
a  mono-acid  base. 

Urea  can  also  be  produced  from  inorganic  sources,  and 
it  was  the  discovery  of  its  synthesis  from  potassium  cyanide 
by  Wohler  in  1827  which  caused  the  abandonment  of  the 
old  view  that  compounds  containing  carbon,  with  the  ex- 
ception of  its  oxides,  belonged  to  a  special  class,  and  could 
be  produced  only  by  the  intervention  of  "life-power."  Its 
production  is  as  follows  :  Potassium  cyanide  is  heated  to 
redness  with  lead  oxide;  KCN  +  PbO  =  KCNO  +  Pb. 
The  cyanate,  KCNO,  is  next  dissolved  and  mixed  with  a 
solution  of  ammonium  sulphate,  and  the  mixture  is  evapo- 
rated to  dryness.  It  may  be  supposed  that  potassium 
sulphate  and  ammonium  cyanate  are  first  formed:  2 KCNO 
+  (NH4)2SO4  =  K2SO4  +  (NHJCNO.  But  the  latter 
compound  is  unstable,  and  undergoes  change  into  its 
isomeride,  urea  :  (NHJCNO  =  O=C(NH2)2.  On  treat- 
ment with  alcohol,  insoluble  potassium  sulphate  remains 
undissolved,  while  the  soluble  urea  crystallises  from  the 
alcohol  on  evaporation.  Urea  is  also  produced  when  carbonyl 
chloride  or  when  ethyl  carbonate  is  treated  with  aqueous 


AMIDES  OF   PHOSPHORUS  175 

ammonia  :  O=CC10  +  2NH3  =  O=C(NH2)0.HC1  + 
HC1  ;  0=C(OC?H5)?  +  2NH3  -  Q-C(NH2)2.  + 
2C9H5OH.  Lastly,  carbamate  of  ammonium,  when  heated 
in  a  sealed  tube,  loses  water  with  formation  of  urea : 
H2N-CO-ONH4  -  0=C(NH2)2  +  H20. 

Bill  ret. — When  urea  is  heated,  a  body  named  biuret  is 
formed,  with  loss  of  one  molecule  of  ammonia.  We  are  here 
reminded  of  the  relation  between  an  acid  and  an  anhydro- 
acid  ;  this  is  evident  on  inspection  of  the  formulas : — 

H2N-CO-NH2  HO-S02-OH 

Urea.  Sulphuric  acid. 

H2N-CO-NH-CO-NH2      HO-SO2-O-SO2-OH 

Biuret.  Anhydrosulphuric  acid. 

Amides  of  Acids  of  Phosphorus. — Many  com- 
pounds analogous  to  urea  are  known,  where  the  hydroxyl 
groups  of  acids  are  replaced  by  amide-groups,  — NH2.  By 
the  action  of  ammonia  gas  on  phosphorus  oxychloride 
ortho-phosphamide  is  formed  :  O=PC13  +  3HNH2  = 
O=P(NH2)3  +  3HC1.  The  ammonium  chloride  formed  by 
the  combination  of  the  hydrochloric  acid  with  excess  of 
ammonia  is  removed  by  washing,  and  an  insoluble  white 
powder  remains.  When  phosphamide  is  heated,  ammonia 
is  lost,  and  phosphoryl-amide-imide  (the  group  =NH 
is  termed  the  "  imido-group "),  HN=PO(NH2),  and  at 
a  higher  temperature,  N=P=O  or  phosphoryl  nitride  are 
left.  They  are  also  white  insoluble  powders.  By  analogy 
with  carbamic  acid  and  urea,  there  should  exist  compounds 
in  which  both  hydroxyl  and  the  amido-group  are  present. 
Some  such  compounds  are  known.  Thiophosphamic 
acid,  S=P(NH2)(OH).2,  is  the  product  of  the  action  of 
ammonia  on  thiophosphoryl  chloride  ;  and  phosphoric 
anhydride,  when  dry  ammonia  gas  is  passed  over  it,  yields 

o. 

phosphimic  acid,  thus :  P9Or  +  zNIHL  = 


176  MODERN   CHEMISTRY 

+  H,O.         It     is     analogous     to     metaphosphoric     acid, 

ov 

^P  —  OH,    and    forms    crystalline    salts.       Pyrophos- 

o^ 

phamic  acids  are  also  known.  The  addition  of  phos- 
phoryl  chloride  to  a  cold  saturated  solution  of  ammonia 
results  in  the  formation  of  pyrophospho-  diamic  acid 


(PO)  —  O  —  (PO)<^         ,  analogous  to  pyrophos- 
H,N/  X)H 

HOX  /OH 

phoric    acid,  >(PO)—  O—  (PO)<  ;     and    on 

HO/  \OH 

heating  the  solution  of  this  body,  one  hydroxyl  group 
replaces  one  amido-group,  yielding  pyrophosphamic  acid, 
H0N,  /OH 

\(PO)—  O—  (PO)<  .      Lastly,  the  action  of 

HO/  X3H 

ammonia  on  phosphoric  chloride  gives  a  compound  named 
phospham,  HN^P^N,  a  species  of  anhydride,  but  pro- 
duced by  loss  of  ammonia,  not  of  water,  from  the  unknown 
compound  P(NH2)_. 

Analogues  of  phosphorous  acid  are  less  well  known  ;  if 
ammonia  be  passed  over  phosphorous  chloride,  a  white  mass 
is  formed,  which  has  not  been  separated  from  ammonium 
chloride,  but  which  is  supposed  to  possess  the  formula 
P(NH2)3;  it  may  be  named  phosphorosamide. 

.A/n/cfes  of  Sa/p/lt/r  Ac/c/S.  —  Similarly,  amido- 
derivatives  can  be  obtained  from  sulphur  trioxide.  The 
action  of  ammonia  on  that  compound  yields  ammonium 
sulphamate,  H4N—  O—  (SO2)—  NH2,  or,  if  less  ammonia 
be  used,  sulphamic  acid,  HO—  (SO0)—  NH2  ;  they  are 
both  crystalline,  soluble  compounds. 

The  action  of  sulphur  dioxide  on  ammonia  is  accompanied 
by  the  production  of  the  analogous  compounds,  ammonium 
sulphurosamate  and  sulphurosamic  acid,  the  latter  of 
which  has  the  formula  RO-(SO)-NH2. 


COMPLEX  AMINES  177 

These  compounds  may  be  taken  as  instances  of  bodies 
analogous  to  acids,  in  which  the  hydroxyl  is  replaced  by 
the  amido-group.  They  are,  as  a  rule,  stable  in  presence 
of  water,  and  they  do  not  generally  unite  with  acids,  the 
acid  nature  of  the  oxygen  which  they  contain  counteracting 
the  basic  nature  of  the  amido-group.  Many  compounds 
are  however  known,  in  which  the  amido-group  replaces 
hydroxyl,  and  which,  having  no  acidic  oxygen  present,  are 
known  only  as  salts  in  combination  with  acids.  Some  of 
these  will  now  be  described. 

Salts  of  Complex  Amines.  —  Calcium  chloride, 
exposed  to  a  stream  of  ammonia  gas,  rapidly  absorbs  it, 
and  forms  the  compound  CaCl2.8NH3.  It  would  appear 
that  this  compound  is  one  of  calcamine,  Ca(NH9)9,  with 
2HC1,  with  which  six  molecules  of  ammonia  are  associated 
in  some  manner  resembling  that  in  which  water  of  crystal- 
lisation is  associated  in  salts  containing  it.  Thus  we  have 
CaCl9.6H9O  ;  and  Ca(NH3)9Cl.2.6NH3  has  an  analogous 
formula.  Zinc  and  cadmium  form  similar  compounds, 
and  other  salts  may  be  obtained  from  the  appropriate  salts 
of  the  metals ;  thus,  by  saturating  zinc  sulphate  with 
ammonia,  the  compound  Zn(NH3)9SO4.H9O  separates 
in  crystals.  Again,  with  aluminium,  A1(NH3)3C13  has 
been  prepared  ;  and  dyad  iron,  manganese,  and  nickel 
yield  somewhat  similar  compounds.  Such  bodies  must 
be  regarded  as  salts  of  ammonium,  in  which  a  metal 
has  taken  the  place  of  one  atom  of  hydrogen  in  each 
molecule  of  ammonium  ;  a  dyad  metal  replacing  two 
metals  in  two  molecules  of  ammonium,  a  triad  three, 
and  so  on. 

The  state  of  such  compounds  in  solution  is  probably 
that  of  "double  salts,"  alluded  to  on  pp.  10  and  161. 
While  some  of  them  are  decomposed  by  water  into  ammonia 
and  the  salt  of  the  metal,  others  resist  that  decomposition, 
and  are  ionised  into  complex  groups,  analogous  to  the  platini- 
chloride  or  the  silicifluoride  group.  Thus,  while  it  is 
probable  that  the  compound  of  ammonia  with  calcium 


178  MODERN   CHEMISTRY 

+  + 

chloride   in   solution    contains   as   ions   Ca,  Cl,  NH4,  and 

OH,  together  with  non-ionised  NH4OH  and  molecular 
NH3,  the  fact  that  zinc  hydroxide,  precipitated  by  addition 
of  ammonium  hydroxide  to  a  solution  of  the  chloride,  is 
re-dissolved  by  further  addition  of  ammonia,  is  doubtless 
to  be  explained  by  the  formation  of  the  complex  ion 
Zn(NH3)2,  which  is  soluble  in  water.  But  this  does  not 

+  + 

exclude  the  presence  of  the  usual  ions,  Zn,  Cl,  NH4,  and 

OH,  which  doubtless  co-exist  with  those  already  mentioned. 
In  some  cases,  the  stability  of  the  complex  ions  is  much 
greater  than  in  that  mentioned,  and  of  this  some  instances 
will  be  given. 

Chromamines.  —  Chromium  hydroxide,when  digested 
with  excess  of  ammonia  and  ammonium  chloride,  forms  a 
deep  red  solution  ;  and  on  exposing  it  to  air,  a  violet 
powder  separates,  of  the  formula  CrCl3.4NH3.H9O.  This 
powder,  heated  to  100°,  loses  its  water  of  crystallisation, 
and  the  residue  has  the  formula  CrCl3.4NH3.  The 
ammonia  is  not  expelled  until  the  temperature  200°  is 
reached.  It  would  appear,  therefore,  that  this  compound 
is  not  Cr(NH3)3.Cl3.NH3,  the  fourth  molecule  of  ammonia 
being  regarded  as  of  the  same  nature  as  water  of  crystallisa- 
tion ;  it  must  rather  be  supposed  that  a  complex  ammonium 
group,  —  NH3—  NH3,  is  capable  of  existence  ;  whence  the 


^ 
compound  would  have  the  formula  Crc  —  NH0  —  NH0  —  Cl. 

\NH'-CI  ' 

Salts  containing  chromium  have  been  prepared,  in  which 
3,  4,  5,  6,  and  7  molecules  of  ammonia  are  associated  with 
the  original  chromium  salt.  They  find  their  explanation 
by  a  hypothesis  like  the  one  given. 

Cobaltamines.  —  Similar  compounds  are  known  with 
triad  cobalt.  On  adding  a  solution  of  ammonia  to  cobalt 
sulphate,  the  precipitate  at  first  formed  (a  basic  sulphate) 


AMINES  179 

dissolves  ;  exposure  to  air  causes  the  oxidation  of  the  cpbalt 
from  dyad  to  triad,  and  a  black  powder  is  deposited.  On 
careful  addition  of  hydrochloric  acid,  keeping  the  mixture 
cold,  the  colour  of  the  powder  changes  to  red  ;  the  com- 

/NH3— Cl 
pound  has  the  formula  Coc-NIHL — NH, — C1.H0O,  and  is 

\NH3— Cl    ' 

analogous  to  the  chromium  compound  mentioned  above. 
Other  salts  of  this  base  have  been  made  ;  they  are  termed 
roseo-cobaltamines.  If  temperature  be  allowed  to  rise, 
during  the  addition  of  hydrochloric  acid  to  the  oxidised 
solution  of  cobalt  sulphate  in  ammonia,  an  isomeric  substance 
is  produced,  containing  no  water  of  crystallisation,  and 
having  a  purple  colour.  Other  salts  are  known  ;  they  are 
termed  salts  of  purpureo-cobaltamine.  It  is  possible  to 
represent  the  formulas  of  such  compounds  as  follows  : — 

Diamines:   Cl-Co(NH3)2Cl.,. 
Triamines  :   Co  (NH« )  £ly 
Tetramines  :   Cl-Co(NH3-NH3)9Cl9. 
Pentamines :   NH9-Co(NH-3NH3).;Cl3. 
Hexamines:   Co(NH3-NH3)3Cl3. 

Other  Amines. — Many  compounds  of  copper,  mer- 
cury, silver,  gold,  and  the  metals  of  the  platinum  group 
are  known,  which  admit  of  representation  in  a  similar 
manner.  They  differ,  however,  inasmuch  as  the  metal 
must  be  considered  to  have  replaced  more  than  one  atom  of 
hydrogen  in  one  molecule  of  ammonium.  Thus  we  have  : 

Cu'2=NH2Cl,  di-cuprosammonium  chloride,  a  black 
powder  produced  by  the  action  of  ammonia  gas  on  warmed 
cuprous  chloride  : 

Cu'— NH3C1,  cuprosammonium  chloride,  formed  by 
dissolving  cuprous  chloride  in  ammonia  ;  it  is  a  well-known 
absorbent  for  carbon  monoxide  and  for  acetylene. 

Cu"=(NH3)9Cl9,  cuprammoniuin  chloride,  and  cupri- 
diammonium  sulphate,  Cu"=(NH3— NH3)9SO4,  the 
former  a  green  substance,  the  latter  a  deep  blue  compound  ; 


iSo  MODERN   CHEMISTRY 

both  produced  by  the  action  of  ammonia  on  the  respective 
cupric  salt.  The  formation  of  the  latter  is  a  well-known 
test  for  copper. 

With  silver  there  are :  Argentamine,  a  black  ex- 
plosive powder,  probably  of  the  formula  AgNH«,  produced 
by  adding  ammonia  to  silver  hydroxide ;  and  numerous 
compounds  of  formulas  like  Ag(NH3)Cl,  produced  by 
dissolving  the  respective  silver  salts  in  ammonia.  With 
gold :  Auric  chloride,  digested  with  ammonia,  yields 
"fulminating  gold,"  an  explosive  black  substance,  which  is 
a  mixture  of  HN= AuCl  and  HN=Au-NH.,. 

A  familiar  test  for  mercurous  mercury  is  to  add  ammonia, 
when  the  compound  turns  black.  This  is  due  to  the 
formation  of  di-mercurosammonium  chloride,  or  some 
similar  compound,  of  the  formula  Hg'0=NH2Cl,  where  two 
atoms  of  hydrogen  in  ammonium  chloride  are  replaced  by 
twro  atoms  of  monad  mercury.  It  has  long  been  known, 
too,  that  mercuric  salts  produce  a  white  precipitate  on  treat- 
ment with  ammonia.  This  is  chiefly  due  to  the  formation  of 
chloro-mercuramine,  Cl  —  Hg"  —  NH2 ;  here,  the  presence 
of  electro-negative  chlorine  deprives  the  amido-group  of 
basic  properties.  On  boiling  this  compound  with  ammo- 
nium chloride,  mercurammonium  chloride  is  produced: 
Cl-Hg-NH2  +  NH4Cl  =  Hg(NH3)2Cl,. 

With  platinum,  and  the  other  members  of  that  group, 
similar  compounds  are  produced ;  but  their  constitution  can 
be  inferred  sufficiently  from  what  has  preceded. 

These  compounds  are  derivatives  of  ammonia  ;  there  are 
few  similar  compounds  of  phosphine ;  one,  however,  is 
produced  when  phosphoretted  hydrogen  is  passed  over 
aluminium  chloride;  its  formula  is  PH^AlClg.  And 
arsine,  passed  through  a  solution  of  mercuric  chloride,  yields 
Hg9AsCl.HgCl2  ;  it  is  somewhat  analogous  to  the  black 
precipitate,  Hg2NH.HCl. 

Phosphides,  Arsenides,  and  Antimonides. — A 
few  compounds  of  phosphorus,  arsenic,  and  antimony  with 
metals  have  been  made.  They  are  generally  obtained  by 


PHOSPHIDES,    ETC.  181 

direct  union  between  the  heated  metal  and  the  element. 
Thus,  if  sodium  and  phosphorus  be  heated  together  under 
xylene,  a  hydrocarbon  boiling  about  130°,  a  black  com- 
pound is  formed,  NagP,  from  which  excess  of  phosphorus 
can  be  dissolved  out  by  treatment  with  carbon  disulphide. 
Arsenide  and  antimonide  of  sodium  are  also  obtained  by 
heating  the  elements  together.  The  formulas  of  these 
compounds  are  of  the  type  AsNa3  ;  and  with  dilute  acid, 
the  corresponding  hydride  of  phosphorus,  arsenic  or  antimony 
is  evolved  :  AsNa3  +  3HCl.Aq  =  AsH3  +  3NaCl.Aq. 
A  mixture  of  calcium  phosphide,  Ca3P2,  with  calcium 
pyrophosphate  is  produced  on  throwing  phosphorus  into  a 
crucible  containing  red-hot  lime  ;  on  treatment  with  water, 
spontaneously  inflammable  phosphine  is  evolved.  The 
spontaneous  ignition  is  due  to  its  containing  P0H4,  a  liquid, 
very  unstable  compound. 

The  phosphides,  arsenides,  and  antimonides  of  the 
other  metals  are  usually  dark-coloured  substances,  with 
more  or  less  metallic  lustre,  and  therefore  conductors  of 
electricity.  Some  of  them  occur  native ;  for  example, 
smaltine,  CoAs2,  a  common  ore  of  cobalt,  forming  silver- 
white  crystals  ;  copper-nickel,  NiAs,  red  lustrous  crystals, 
and  one  of  the  chief  nickel  ores  ;  speiss,  a  deposit  formed 
in  the  pots  in  which  smaltine  and  copper-nickel  are  fused 
with  potassium  carbonate  and  silica,  in  the  preparation  of 
smalt,  a  blue  glass  containing  cobalt ;  its  formula  appears  to 
be  Ni3As2.  Mispickel,  or  arsenical  pyrites,  is  a  white 
lustrous  substance,  of  the  formula  FeSAs. 

Cyanides. — The  elements  carbon  and  nitrogen  form  a 
very  stable  group,  of  which  the  compounds  have  been  well 
investigated,  termed  cyanogen.  Carbon  and  nitrogen  do 
not  unite  directly  ;  but  if  a  mixture  of  finely  divided  carbon 
with  carbonate  of  potassium  or  sodium,  or,  better,  of  barium, 
be  heated  to  about  1 200°  in  a  current  of  nitrogen,  combina- 
tion ensues,  and  a  cyanide  is  formed,  KCN,  NaCN,  or 
Ba(CN)2;  BaC03  +  4C  +  N2  =  Ba(CN)2  +  3CO.  Potas- 
sium cyanide  is  also  produced  when  a  mixture  of  animal 


i82  MODERN   CHEMISTRY 

refuse  (horns,  hides,  hair,  dried  entrails,  &c.,  of  animals) 
with  potassium  carbonate  and  iron  filings  is  heated.  The 
nitrogen  of  the  animal  matter  and  the  carbon  unite  with  the 
potassium  of  the  carbonate,  forming  cyanide.  On  addition 
of  water,  this  cyanide  reacts  with  salts  of  iron,  forming  a 
double  cyanide  of  iron  and  potassium,  termed  "  yellow 
prussiate  of  potash,"  or  ferrocyanide  of  potassium,  of  the 
formula  K4Fe(CN)6.  When  this  compound  is  heated  to 
dull  redness,  it  fuses  ;  a  black  mixture  or  compound  of  iron 
and  carbon  remains,  and  melted  potassium  cyanide  can  be 
poured  out  of  the  crucible.  Potassium  cyanide,  KCN,  is  a 
very  soluble  salt ;  it  crystallises  well  from  alcohol.  Its 
solution  smells  of  hydrocyanic  acid  ;  this  is  because  it  is 
hydrolysed  by  water.  The  acid,  HCN,  is  so  very  weak 
that  the  number  of  hydrogen  ions  present  in  its  solution  are 
comparable  in  number  with  those  of  ionised  water  ;  hence 

the  change:  H-OH  +  K-CN.Aq=HCN  +  KOH.Aq. 
The  ionised  portion  of  the  hydrocyanic  acid  is  as  usual  non- 
volatile ;  but  the  non-ionised  portion  has  a  vapour-pressure, 
and  can  be  detected  by  its  smell  (cf.  p.  141). 

Hydrocyanic  Acid. — Inasmuch  as  hydrocyanic  or 
"  prussic  "  acid  is  so  very  weak,  it  is  displaced  from  its 
salts  by  the  action  of  all  other  acids  ;  even  carbonic  acid 
can  expel  it.  It  may  therefore  be  prepared  by  distilling  a 
cyanide  (potassium  cyanide  or  ferro-cyanide  is  generally 
used)  with  dilute  sulphuric  acid.  The  vapour  comes  off 
along  with  water  ;  to  remove  the  water,  if  the  anhydrous  acid 
is  required,  the  mixture  of  vapours  may  be  passed  through 
a  tube  charged  with  dry  calcium  chloride,  which  retains 
the  water  ;  or  by  another  method,  mercuric  cyanide  may  be 
decomposed  by  passing  over  it  a  current  of  dry  sulphuretted 
hydrogen,  the  excess  of  which  is  removed  by  causing  the 
gases  to  traverse  a  tube  filled  with  lead  carbonate ;  the 
hydrocyanic  acid  must  be  condensed  in  a  freezing-mixture, 
for  it  boils  at  27°.  The  solid  compound  melts  at  -I  5°.  All 
experiments  with  anhydrous  or  with  concentrated  hydrocy- 


ISOMERIC   CYANIDES  183 

anic  acid  must  be  carried  out  in  a  good  draught-chamber, 
for  it  is  the  most  poisonous  substance  known,  and  a  breath 
of  its  vapour  has  been  attended  by  fatal  effects. 

The  cyanides  are  produced  by  addition  of  the  oxides  or 
hydroxides  to  hydrocyanic  acid.  Those  of  the  alkalies 
and  alkaline  earths  are  white,  soluble  crystalline  com- 
pounds ;  those  of  lead,  mercury,  and  silver  closely  resemble 
the  chlorides.  Mercuric  cyanide,  a  sparingly  soluble, 
white  crystalline  salt,  is  formed  by  dissolving  mercuric  oxide 
in  hydrocyanic  acid ;  lead  cyanide  is  also  sparingly  soluble, 
and  silver  cyanide,  produced  by  addition  of  potassium  cyanide 
to  a  soluble  silver  salt,  is  an  insoluble  white  precipitate,  un- 
distinguishable  from  silver  chloride  in  appearance.  The 
cyanide  of  silver  or  of  mercury,  when  heated,  yields  cyanogen, 
(CN)2,  a  colourless  gas,  possessing  the  characteristic  cyanide 
smell,  somewhat  resembling  that  of  bitter  almonds.  Like 
hydrocyanic  acid,  it  is  very  poisonous.  It  burns  with  a 
blue-purple  flame ;  it  is  fairly  soluble  in  water  and  in 
alcohol.  It  condenses  to  a  liquid  which  boils  at  —  20°, 
and  freezes  at  —  34.4°.  It  is  an  endothermic  substance, 
being  formed  from  its  elements  with  an  absorption  of  heat 
of  —  65,700  calories. 

Isomeric  Cyanides. — The  formula  of  hydrocyanic 
acid  can  be  represented  in  two  ways.  It  is  possible  to 
conceive  either  the  carbon  or  the  nitrogen  to  be  united 
with  the  atom  of  hydrogen.  In  the  former  case,  the 
structural  formula  is  H— C^N  ;  in  the  latter,  H— N=C. 
There  is  no  method  of  determining  which  of  the  two 
formulae  is  to  be  ascribed  to  the  acid  or  to  its  simple  salts  ; 
but  salts  with  alcohol  radicals  are  known  to  which  one  or 
other  formula  can  be  ascribed.  On  distilling  potassium 
cyanide  with  potassium  ethyl-sulphate,  the  following  change 
takes  place :K-C=N  +  C2H5.KSO4  =  CH3-CH2-C^N 
4-  K2SO4.  Here  it  is  known  that  the  carbon  of  the  ethyl 
group  is  in  direct  union  with  the  carbon  of  the  cyanogen 
for  two  reasons  :  first,  when  ethyl  cyanide  is  exposed  to 
the  action  of  nascent  hydrogen  (e.g.  treated  with  tin  and 


1 84  MODERN   CHEMISTRY 

hydrochloric  acid)  hydrogen  adds  itself  both  to  the  carbon 
and  to  the  nitrogen  of  the  cyanide  group,  and  propyl- 
amine,  CH3— CH2— CH2— NH9,  is  formed  ;  and  second,  on 
boiling  ethyl  cyanide  with  a  solution  of  caustic  potash 
in  alcohol,  an  acid  with  three  carbon  atoms,  propionic 
acid,  is  formed  :  CH3-CH2-C=N  +  KOH  +  H0O  = 

J* 

CH3— CH2— C^          +  NH3  ;     dyad   oxygen   and   monad 

\OK 

potassoxyl  replace  triad  nitrogen.  On  the  other  hand,  if 
ethyl  iodide,  CHg— CH9— I,  be  boiled  in  alcoholic  solution 
with  silver  cyanide,  the  changeis :  CH3— CH2— I  +  Ag— N=C 
=  CH3— CH2— N=C  +  Agl.  Here  the  nitrogen  is  in  direct 
union  with  the  carbon  atom  of  the  ethyl  group  ;  this  is  known 
because  on  boiling  the  compound  with  dilute  acid,  hydro- 
lysis takes  place,  thus:  CHg-CH2-N=C  +  2H0O  = 
CH3-CH2-NH2  +  H-CO-OH;  the  nitrogen  remains 
in  union  with  the  carbon.  Hence  it  is  concluded  that 
while  potassium  cyanide  must  contain  K— C=N,  along  with 
K— N=C  (for  both  compounds  are  formed  by  the  first 
action),  silver  cyanide  consists  almost  exclusively  of 
Ag— N=C.  The  name  applied  to  the  first  compound, 
CH3CH9CN,  is  ethyl  cyanide,  or,  preferably,  propionitrile, 
seeing  that  it  differs  from  propionic  acid  only  in  having 
nitrogen  in  place  of  oxygen  and  hydroxyl ;  while  the  latter 
is  turned  ethyl  isocyanide  or  ethyl  carbamine,  for  it  contains 
carbon  replacing  hydrogen  in  ethylamine,  CHgCH0— NH0. 

Hydrocyanic  acid  may  on  the  same  grounds  be  termed 
"  formonitrile,"  for,  on  standing  with  dilute  acid,  it  is 
converted  into  formic  acid  by  assumption  of  the  elements 
of  water:  H-C-N  +  2H2O  =  H-CO-OH  +  NHg;  and 
cyanogen,  for  the  same  reasons,  may  be  named  "  oxaloni- 

C=N  CO-OH 

trile":    |          +  4H2O  =     \  +  2NH 

C=N  CO-OH 

Ferro-  and  Ferricyanides* — Some  of  the  double 
cyanides  are  of  importance,  both  commercially  and  from  a 


FERROCYANIDES  185 

chemical  standpoint.  Among  them  is  a  substance  which 
has  already  been  mentioned,  potassium  ferrocyanide, 
K4Fe(CN)6.  This  compound  forms  large  yellow 
tabular  crystals  ;  it  contains  ferrous  iron,  hence  the 
name  ferro(us)cyanide.  It  is  supposed  to  be  derived 
from  a  tricyanogen  group,  and  to  have  the  formula 

K—  C  C—  K 


N  >C—  Fe—  C^         N 

I    JN/  \N.    | 

K—  C^  ^C—  K 

+ 
The  ions   of  this   salt  are  five,  viz.,  4K,  and  the   complex 

group  Fe(CN)6;  the  fall  in  freezing-point  of  an  aqueous 
solution  caused  by  the  presence  of  a  gram-molecule  in 
100,000  parts  of  water,  and  the  conductivity  of  a  similarly 
dilute  aqueous  solution  indubitably  indicate  the  presence  of 
five  ions.  Moreover,  the  salt  shows  none  of  the  reactions 
characteristic  of  ions  of  dyad  iron,  such  as  precipitation  as 
sulphide  on  addition  of  ammonium  sulphide,  precipitation  as 
hydroxide  on  addition  of  alkalies,  &c.  The  acid  corre- 
sponding to  this  salt,  hydroferrocyanic  acid,  H4Fe(CN)6, 
can  be  prepared  by  adding  to  a  boiled  solution  of  potassium 
ferrocyanide  concentrated  hydrochloric  acid  and  a  little 
ether  ;  it  precipitates  in  white  crystals.  The  zinc  salt 
and  the  copper-potassium  salt,  K2CuFe(CN)6,  are  in- 
soluble ;  the  former  is  white,  and  the  latter  a  slimy  brown- 
red  precipitate. 

On  passing  a  current  of  chlorine  through  a  solution  of 
potassium  ferrocyanide,  or  on  submitting  it  to  the  action  of 
any  oxidising  agent,  potassium  ferri(c)  cyanide  is  formed  : 
2K4Fe(CN)6  .  Aq  +  C12  =  KC1  .  Aq  +  2K8Fe(CN)6  .  Aq. 
The  new  compound  contains  ferric  iron,  hence  its  name  ; 
the  "  c  "  is  omitted  for  the  sake  of  euphony.  This 
salt  crystallises  in  dark  red  prisms,  and  dissolves  in  water 
with  an  orange  colour.  The  acid,  prepared  from  the  lead 


1 86  MODERN   CHEMISTRY 

salt,  which  is  sparingly  soluble,  by  the  action  of  dilute 
sulphuric  acid,  and  evaporation  to  crystallising  point, 
forms  brownish  needles.  Here  again  the  complex  group 

-  Fe(CN)6  is  one  of  the  complex  ions  in  solution  along 

+ 

with  3K  ;  and  it  is  to  be  noticed  that  it  now  carries  only 
three  electrons  instead  of  four,  as  in  the  ferrocyanide. 
Similar  instances  are  to  be  remarked  in  elements  of  two 
valencies ;  and  in  the  manganates  and  the  permanganates, 

the  former  of  which  have  the  dyad  ion  MnO4,  while  with 

the  latter  it  is  monad,  MnO4.  The  iron  salts  of  ferro- 
and  ferricyanic  acids  are  especially  interesting,  and  some  of 
them  are  of  commercial  importance.  On  adding  a  solution 
of  ferrocyanide  of  potassium,  boiled  so  as  to  expel  dissolved 
oxygen,  to  a  solution  of  iron  wire  in  sulphurous  acid,  which 
is  also  free  from  dissolved  oxygen,  a  white  precipitate  of 
potassium  ferrous  ferrocyanide  results :  FeSO3.Aq  + 
K4Fe''(CN)6.Aq  =  K2Fe'Te"(CN)6  +  K2SO3.Aq.  If 
these  precautions  to  exclude  oxygen  are  not  taken,  the 
precipitate  is  light  blue  in  colour,  and  is  a  common  test  for 
ferrous  iron.  This  compound  is  also  formed  when  ferro- 
cyanide of  potassium  is  distilled  with  dilute  sulphuric  acid, 
as  in  the  preparation  of  prussic  acid:  2K4Fe"(CN)6.Aq  + 
3H2S04.Aq  =  K2Fe"Fe"(CN)6  +  3K2SO4.Aq.  When 
boiled  with  dilute  nitric  acid,  the  white  compound  is  con- 
verted into  a  blue  soluble  compound,  which  may  be 
regarded  either  as  potassium  ferrous  ferricyanide  or 
potassium  ferric  ferrocyanide,  KFe"Fe'"(CN)6,  or 
KFe'"Fe"(CN)6.  This  same  compound  is  produced  also 
by  the  addition  of  a  ferric  salt  to  potassium  ferrocyanide  : 
K4Fe"(CN)G.Aq  +  Fe"'Cl3.Aq  =  KFe'"Fe"(CN)6.Aq 

+  3KCl.Aq  ;  or  by  adding  a  ferrous  salt  to  potassium  ferri- 
cyanide :  K3Fe///(CN)6.Aq  +  Fe"Cl,.Aq  -  aKCl.Aq 

-I-  KFe"Fe'"(CN)6.  Aq.  When  mixed  with  excess 
of  a  ferrous  salt,  it  gives  a  blue  precipitate  named 


CYANIDES  187 

"Turnbull's  blue":  2KFe"Fe'"(CN)6.Aq  +  Fe''SO4.Aq 
3*sFc/'8Fe"/2(CN),05  and  with  excess  of  a  ferric  salt, 
"Prussian "blue" "is  formed:  3KFe"Fe'"(CN)rt.Aq  + 
Fe'"Cl3.Aq  -  FeyV"4(CN)ls  +  3KCl.Aq.  Potassium 
ferricyanide,  with  ferric  iron,  gives  a  brown  solution,  which 
may  contain  ferric  cyanide.  These  colours  are  used  as  tests 
for  ferric  or  ferrous  iron. 

Chromicyanides,  manganicyanides,  cobalticyanides, 
ruthenocyanides,  and  osmocyanides,  are  also  known, 
similar  in  formulae  to  the  ferro-  and  ferri-cyanides.  On  the 
other  hand,  nickel  and  platinum  form  double  cyanides 
similar  in  formula  to  K0Pt(CN)4.  The  platinum  salts 
are  very  beautiful,  possessing  the  property  of  dichroism,  i.e. 
of  transmitting  light  different  in  colour  from  that  which  the 
crystals  reflect ;  moreover,  only  some  of  the  facets  of  the 
crystals  have  this  property. 

Silver  cyanide  is  soluble  in  a  solution  of  potassium 
cyanide,  also  forming  a  double  salt,  of  the  formula 

KAg(CN)2.  Here  the  ions  are  K  and  Ag~(CN)2. 
This  salt  finds  two  uses.  First,  it  is  the  compound  from 
which  silver  is  best  deposited  electrolytically  in  elec- 
troplating (see  p.  10).  Potassium  auricyanide, 

KAu(CN)4.Aq,  produced  by  the  addition  of  auric 
chloride,  AuClg,  to  a  solution  of  potassium  cyanide,  is 
employed  in  gold-plating.  Second,  the  existence  of  the 
soluble  ion,  Ag(CN)9,  furnishes  a  means  of  estimating  the 
amount  of  hydrocyanic  acid  in  a  dilute  solution  such  as  is 
used  for  medicinal  purposes.  A  decinormal  solution  of 
silver  nitrate,  that  is,  one  containing  one-tenth  of  the  mole- 
cular weight  of  the  salt  taken  in  grams,  or  17  grams  per 
litre,  will  react  with  13.02  grams  of  potassium  cyanide, 
or  with  5.4  grams  of  hydrocyanic  acid,  forming  the 
double  salt,  thus:  AgNO3.Aq  +  2KCN.Aq  =  KNO3.Aq 

170  J30.2 

+  KAg(CN)2.Aq.  The  solution  of  silver  nitrate  is  added 
from  a  measuring-tube  or  burette  until  a  faint  trace  of 


i88  MODERN   CHEMISTRY 

turbidity  begins  to  appear  ;  this  signifies  that  the  reaction 
given  above  has  completed  itself,  and  that  the  second 
reaction— KAg(CN)2.Aq  +  AgNO3.Aq=KNO3.Aq  + 
2AgCN — has  just  begun.  Every  cubic  centimeter,  there- 
fore, of  silver  nitrate  added  corresponds  to  the  presence  of 
0.0054  grams  of  hydrocyanic  acid  in  solution. 

Metallic  gold  is  soluble  in  a  dilute  solution  of  potassium 
or  sodium  cyanide,  the  complex  group  Au(CN)3  being 
formed,  thus  : — 

4KCN.  Aq  +  Au  =  KAu(CN)4.  Aq  +  K. 

The  action  of  the  potassium  on  the  water  is  to  liberate 
hydrogen.  But  this  hydrogen  attacks  the  oxygen  dissolved 
in  the  water,  and  is  removed  by  water.  The  process  is 
largely  used  in  recovering  gold  from  poor  gold  ores,  or 
from  the  "  slimes,"  or  mud  left  after  removing  the  bulk  of 
the  gold  from  the  crushed  ore,  by  amalgamating  it  with 
mercury. 

The  addition  of  a  solution  of  potassium  cyanide  to  a 
solution  of  a  cupric  salt  in  ammonia,  which,  it  will  be 
remembered,  contains  the  blue  ions  of  the  cupramine, 

+    + 
Cu(NH3)2,  decolorises  the  solution.      This  is  due  to  the 

formation  of  the  double  salt,   potassium    cupricyanide, 

+ 

K2Cu(CN)4.Aq,  the  ions  of  which  are  colourless.      The 

+  + 

copper  is  not  present  in  the  form  of  cupric  ions,  Cu,  hence 
it  does  not  give  the  reactions  characteristic  of  these  ions. 
For  example,  it  yields  no  precipitate  with  sulphuretted 
hydrogen  ;  and  this  affords  a  means  of  separating  copper 
from  cadmium,  which  is  unaffected  by  addition  of  potas- 
sium cyanide. 


CHAPTER  X 

Borides  and  Carbides — Alloys:    their  classifi- 
cation— The  commoner  Alloys. 

Borides  and  Carbides. — These  compounds  have 
been  incidentally  mentioned  on  p.  30  ;  they  have  been  in- 
vestigated almost  exclusively  by  Moissan  and  his  pupils. 

Borides. — Calcium,  strontium,  and  barium  borides 

have  been  prepared  by  heating  in  an  electric  furnace  a 
mixture  of  borate  of  the  metal  with  aluminium  filings  and 
carbon.  At  the  high  temperature  of  the  electric  arc  the 
carbon  reduces  the  aluminium  oxide  and  prevents  its 
formation.  These  compounds  form  hard,  transparent 
microscopic  cubes,  burning  only  when  maintained  at  a 
red  heat  in  oxygen,  and  attacked  with  difficulty  by  the 
halogens.  Their  formulae  are  curious ;  they  are  analogous 
to  the  very  unstable  hydrazoates,  M'(N)3,  being  Ca(B3)2, 
Sr(B3)2,  and  Ba(B3)0;  and  their  existence  would  point  to 

/B 

a  supposititious  compound  of  the  formula  H — B<^   ||    like 

\B 
/N 

H— N<   || . 
\N 

Ferric  boride,  produced  by  heating  together  boron  and 
wrought-iron  in  an  electric  furnace,  consists  of  brilliant 
yellowish-grey  crystals,  burning  brilliantly  when  heated  in 
oxygen,  and  attacked  by  nitric  acid.  The  corresponding 
compounds  of  nickel  and  cobalt,  prepared  in  the  same 


190  MODERN   CHEMISTRY 

manner,  form  brilliant  prisms.  The  formulae  are  FeB, 
NiB,  and  CoB. 

Carbon  boride,  CB6,  forms  lustrous  black  crystals, 
nearly  as  hard  as  diamond,  on  which  facets  can  be  cut  by 
its  use  ;  it  is  produced  by  heating  a  mixture  of  amorphous 
boron  and  sugar-charcoal  in  the  electric  furnace. 

Carbides.  —  Lithium  carbide,  Li2C2,  is  a  white 
crystalline  mass,  produced  by  heating  in  the  electric 
furnace  a  mixture  of  carbon  with  lithium  carbonate  ;  its 
formation  is  expressed  by  the  equation:  Li9CO3  +  4C  = 
Li9C9  +  3CO.  It  is  decomposed  at  a  temperature  not 
much  higher  than  that  at  which  it  is  formed  ;  hence  the 
exposure  to  the  high  temperature  of  the  electric  furnace 
should  be  only  a  short  one.  The  analogous  compounds  of 
sodium  and  potassium  do  not  resist  such  a  high  tempera- 
ture ;  they  must  therefore  be  prepared  by  exposing  the 
metal  for  several  weeks  to  the  action  of  acetylene  under 
pressure.  This  process  yields  compounds  of  the  formulas 
NaHC9  and  KHC2  ;  when  heated,  they  change,  with 
evolution  of  acetylene,  into  the  carbides  Na2C2  and  K0C0. 
Like  lithium  carbide,  they  are  white  crystalline  substances, 
and  with  water  acetylene  is  evolved  :  Na2C2  +  2H2O  = 


Calcium  carbide,  CaC9,  has  attained  great  industrial 
importance  owing  to  its  serving  as  the  source  of  acetylene, 
now  largely  used  for  illuminating  purposes.  It  was  made 
in  an  impure  state  in  1892  by  Travers  by  heating  to- 
gether a  mixture  of  calcium  chloride,  carbon,  and  sodium  ; 
but  it  is  best  produced  by  Moissan's  process  in  the  electric 
furnace,  by  heating  a  mixture  of  carbon  and  lime  to  the 
very  high  temperature  (about  3000°)  obtained  in  that 
manner.  It  forms  blackish-grey,  lustrous  crystals,  at  once 
attacked  by  water:  CaC2  +  2HOH  =  C2H2  +  Ca(OH)2. 
Carbides  of  strontium  and  barium  are  ma  Je  in  a  similar 
manner,  and  have  properties  analogous  to  those  of  the 
calcium  compound. 

Other   carbides  prepared    by  Moissan  in  a  crystalline 


CARBIDES  191 

state  by  means  of  the  electric  furnace  are  :  CeC9,  LaC9, 
YC0,  ThC.,,  which  yield  with  water  a  mixture  of  acetylene, 
ethylene,  methane,  and  hydrogen  ;  Al4Cg,  which  is  decom- 
posed by  water,  yielding  pure  methane  ;  MnyC,  yielding 
methane  and  hydrogen  ;  and  U2C3,  the  products  from  which 
are  ethylene,  methane,  and  hydrogen.  By  heating  the  oxide 
of  the  respective  metal  with  calcium  carbide,  the  carbides 
Cr3C,,  Mo.2C,  W2C,  TiC,  and  SiC  have  also  been 
prepared.  The  last  of  these  has  become  known  com- 
mercially under  the  name  "carborundum."  It  forms 
extremely  hard,  blackish-blue,  hexagonal  crystals ;  when 
pure  it  is  colourless.  It  is  prepared  on  a  large  scale  by 
heating  together  in  the  electric  furnace  a  mixture  of  car- 
bon (coke)  and  white  sand.  It  is  used  for  grinding  and 
polishing  metals  and  glass. 

Steel,  as  is  well  known,  differs  from  iron  by  the  presence 
of  a  certain  amount  of  carbon,  which  induces  the  iron, 
when  cold,  to  persist  in  its  allotropic  state.  This  appears 
to  be  due  to  a  carbide  of  iron  mixed  with  the  excess  of 
iron  in  the  steel.  The  compound  has  been  found  as  a 
meteoric  mass ;  it  has  been  named  cohenite,  and  has  the 
formula  Fe3C.  On  treating  steel  with  dilute  acetic  acid, 
the  same  substance  remains  as  a  black  powder.  Its  for- 
mula is  similar  to  that  of  manganese  carbide,  MngC. 

Sllicides. — Some  silicides  have  also  been  prepared  by 
aid  of  the  electric  furnace  by  heating  elements  with  silicon. 
Among  these  are  Fe9Si,  lustrous  prisms ;  Cr.7Si,  Ni2Si, 
Co2Si,  Mn9Si,  Cu0Si,  and  Pt2Si,  with  similar  properties. 
Magnesium  silicide,  Mg9Si,  prepared  by  heating  a  mixture 
of  powdered  silica  and  magnesium  dust  to  redness,  is 
attacked  by  dilute  acid,  evolving  a  mixture  of  hydrogen 
and  hydrogen  silicide  (see  p.  38). 

Alloys. — The  word  "alloy"  was  originally  applied  to 
mixtures  of  gold  and  silver  with  other  metals ;  it  now 
signifies  any  mixture  or  compounds  of  metals  with  each 
other;  alloys  of  mercury  are,  however,  termed  "amal- 
gams." When  two  metals  are  melted  together,  they 


192  MODERN   CHEMISTRY 

always  mix,  more  or  less.  Some  may  be  mixed  in  any 
desired  proportion,  such  as  lead  and  tin  ;  others  are  par- 
tially soluble  in  each  other ;  zinc,  for  example,  dissolves 
1.6  per  cent,  of  lead,  and  lead  1.2  per  cent,  of  zinc  ;  but 
.  on  stirring  up  the  metals  together,  there  is  always  a  layer 
at  the  top  of  the  lighter  alloy  of  zinc  with  lead,  and  below 
it  the  heavier  alloy,  consisting  chiefly  of  lead.  By  raising 
the  temperature  the  mutual  solubility  of  the  metals  in- 
creases, and  at  a  sufficiently  high  temperature  it  is  probable 
that  they  would  mix  completely. 

Classification. — Alloys  in  general  may  be  classified 
under  two  heads  :  ( I )  definite  compounds,  in  which  the 
elements  are  present  in  atomic  proportions;  and  (2)  mix- 
tures in  which  combination  has  not  taken  place.  To  these 
classes  may  be  added  a  third — mixtures  of  definite  com- 
pounds with  one  or  other  of  the  components  of  the  alloy. 
As  such  mixtures  are  usually  homogeneous,  it  is  often  a 
matter  of  great  difficulty  to  identify  the  definite  compounds. 
In  many  cases,  too,  it  would  appear  that  one  of  the  metals 
in  the  alloy  is  present  in  an  allotropic  form  ;  for  example, 
on  treatment  of  one  of  the  alloys  of  rhodium  and  zinc  with 
dilute  hydrochloric  acid,  after  solution  of  the  zinc,  the 
rhodium  is  left  in  an  allotropic  form. 

The  constitution  of  alloys  can  be  deciphered  by  several 
processes.  One  depends  on  measurement  of  the  electro- 
motive force  of  a  battery  consisting  of  the  alloy  and  a  plate 
of  some  resistant  metal — for  instance,  platinum  —  compared 
with  that  of  a  similar  cell  made  with  one  of  the  con- 
stituents of  the  alloy.  To  take  a  concrete  example. 
Suppose  a  cell  were  constructed  of  a  plate  of  copper  and 
a  plate  of  platinum  dipping  in  some  appropriate  liquid,  a 
certain  electromotive  force  would  result.  Imagine  a  plate 
of  tin  riveted  to  the  face  of  the  copper  plate,  the  electro- 
motive force  would  now  be  that  of  the  more  electropositive 
metal,  tin.  If  a  plate  of  bronze  be  substituted,  supposing 
it  to  contain  free  tin  not  in  chemical  combination  with 
the  copper,  then  the  electromotive  force  will  still  be  that  of 


ALLOYS  193 

tin  against  platinum.  A  chemical  compound  of  tin  and 
copper,  however,  would  have  a  less  electromotive  force 
than  free  tin  ;  and  as  the  tin  in  the  alloy  mentioned  is 
dissolved  away,  the  electromotive  force  will  suddenly  fall 
when  the  excess  of  tin  has  been  dissolved,  until  it  is  equal 
to  that  of  the  chemical  compound  against  platinum.  An 
analysis  of  the  alloy  at  this  stage  will  reveal  the  com- 
position of  the  compound.  In  this  way  the  existence  of 
a  compound  of  the  formula  Cu3Sn  was  detected. 

The  second  method  of  determining  whether  an  alloy 
contains  a  definite  compound  is  to  compare  the  freezing- 
points  of  various  alloys  of  the  metals.  The  presence  of 
a  small  amount  of  one  metal  in  another  in  general  lowers 
the  freezing-point ;  and  the  freezing-point  is  continuously 
lowered  by  successive  additions,  until  the  lowering  reaches 
a  maximum.  The  mixture  which  has  the  lowest  possible 
melting-point  is  termed  the  "  eutectic  "  alloy.  The  com- 
position of  this  alloy  does  not  necessarily  coincide  with  that 
of  a  definite  compound ;  indeed,  metals  which  form  no 
compound  with  each  other  exhibit  this  phenomenon.  If  a 
compound  is  formed,  however,  the  melting-point  rises  to 
a  maximum  on  continuous  addition  of  the  second  metal, 
and  that  compound  which  has  the  highest  melting-point 
corresponds  with  a  definite  formula.  Further  addition  of 
the  second  metal  causes  a  lowering  of  the  freezing-point 
of  the  definite  compound  ;  and  this  lowering  increases  on 
addition  of  the  second  metal,  until  a  second  eutectic  alloy 
is  formed,  one  consisting  of  a  mixture  of  the  compound 
with  excess  of  the  second  metal.  Further  addition  of  the 
second  metal  now  causes  the  melting-point  to  rise,  it  may 
be  to  the  melting-point  of  the  second  metal ;  in  that  case 
only  one  compound  of  the  two  metals  is  capable  of 
existence.  It  may  happen,  however,  that,  after  rising  to  a 
certain  temperature,  the  temperature  again  falls  on  addition 
of  more  of  the  second  metal ;  in  that  case,  the  highest 
temperature  reached  corresponds  to  the  existence  of  a 
second  compound  ;  a  similar  change  may  even  denote  the 

VOL.   II.  N 


194  MODERN   CHEMISTRY 

existence  of  a  third.  By  such  means  it  is  possible  to  de- 
tect the  existence  of  definite  compounds  between  any  two 
metals.  With  ternary  alloys,  i.e.  with  alloys  containing 
three  metals,  although  the  phenomenon  is  more  compli- 
cated, this  method  has  led  to  the  discovery  of  several 
definite  compounds. 

While  alloys  have  generally  been  prepared  by  melting 
the  metals  together,  or  by  melting  one  of  them  and  adding 
the  other,  some  alloys  have  been  produced  by  submitting 
mixtures  of  the  metallic  powders  to  enormous  pressure. 

"Fusible  Alloys." — Among  the  eutectic  alloys,  some 
are  known  as  "fusible  alloys."  "Wood's  alloy"  con- 
sists of  two  parts  of  tin,  two  of  lead,  seven  or  eight  of 
bismuth,  and  one  or  two  of  cadmium;  it  melts  at  66°-7i°; 
an  alloy  melting  at  60°  (Lipowitz's)  consists  of  tin  four 
parts,  lead  eight  parts,  bismuth  fifteen  parts,  and  cadmium 
three  parts. 

Among  the  few  alloys  of  definite  composition  are: 
ZnPt,  Zn3Hg,  Cd2Tl,  Al8Mn,  Sn4Pt,  Cu3Sn,  and  PtHg2. 
Attempts  have  been  made  to  separate  the  constituents  of 
alloys  by  passing  a  current  of  high  potential  through  the 
melted  alloy,  with  the  expectation  that  electrolysis  would 
take  place ;  but  no  sign  of  such  separation  could  be  detected  ; 
the  alloy  conducts  as  a  whole. 

The  following  alloys,  among  others,  find  practical  use: — 

Sodium  amalgam,  made  by  adding  small  pieces  of 
sodium  to  mercury,  warmed  under  a  layer  of  heavy  paraffin 
oil;  it  is  liquid  when  it  contains  under  1.5  per  cent,  of 
sodium,  and  solid  if  it  contains  more.  It  is  used  as  a 
source  of  nascent  hydrogen,  for  it  is  slowly  attacked  by 
water,  and  more  rapidly  by  dilute  acids.  On  adding  this 
alloy  to  a  concentrated  solution  of  ammonium  chloride,  a 
very  remarkable  phenomenon  takes  place ;  the  amalgam 
swells  up  enormously  while  retaining  its  metallic  appear- 
ance ;  the  product  is  soft  and  of  buttery  consistency ;  it 
may  consist  of  ammonium  amalgam,  and  may  contain  the 
complex  group  NH4,  or,  more  probably,  (NH4)2.  On 


ALLOYS  195 

standing,  it  rapidly  decomposes  into  mercury,  ammonia, 
and  hydrogen. 

The  addition  of  a  little  magnesium  to  nickel  lowers 
its  melting-point  considerably,  and  renders  it  ductile  and 
malleable.  A  similar  addition  of  a  little  aluminium  to 
iron  also  improves  the  qualities  of  the  iron.  The  product 
is  called  "  Mitis  steel." 

"  Galvanised  iron  "  is  produced  by  passing  clean  sheets 
of  iron  through  molten  zinc.  Alloying  takes  place  on  the 
surface  of  the  iron.  Such  plates,  in  a  corrugated  form, 
are  largely  used  for  roofing  buildings.  As  zinc  is  a  more 
electropositive  metal  than  iron,  the  iron  is  thereby  pro- 
tected from  rusting.  Iron  is  similarly  coated  with  tin; 
but  in  this  case,  the  iron,  if  exposed,  is  prone  to  rust,  for 
iron  is  more  electropositive  than  tin,  and  is  attacked  by 
carbonic  acid  in  water  more  readily  than  the  tin.  Indeed, 
rusting  proceeds  in  an  accelerated  rate  owing  to  the  presence 
of  the  tin,  for  the  two  metals  form  a  couple. 

To  deprive  commercial  lead  of  the  silver  which  it 
almost  always  contains,  zinc  is  stirred  up  with  the  molten 
metal  ;  the  zinc  dissolves  the  silver  and  floats  to  the 
surface  of  the  lead ;  it  is  allowed  to  harden,  and  the  cake 
is  then  removed.  The  silver  and  zinc  are  separated  by 
distillation  of  the  more  volatile  zinc ;  the  lead  is  freed  from 
zinc  by  melting  it  in  an  oxidising  atmosphere,  when  the 
more  easily  oxidisable  zinc  is  first  oxidised,  and  can  be 
removed  as  dross.  This  is  Parke's  process  for  desilverising 
lead. 

The  alloy  of  zinc  with  copper  is  termed  brass,  pinch- 
beck, Muntz  metal,  and  tombac.  English  brass  usually 
contains  70  per  cent,  of  copper  and  30  of  zinc.  It  is 
made  by  melting  the  copper  and  adding  the  molten  zinc. 
The  addition  of  nickel  (Cu  52  per  cent.,  Zn  23  per  cent., 
Ni  1 5  per  cent. )  yields  "  German  silver,"  of  which  spoons, 
forks,  and  coins  are  made.  Electroplate  has  usually  a  basis 
of  this  alloy,  and  is  covered  with  silver  by  depositing  it 
from  its  double  cyanide  with  potassium.  Zinc  coated  over 


196  MODERN   CHEMISTRY 

with  a  superficial  layer  of  zinc  amalgam  is  not  attacked  by 
dilute  sulphuric  acid,  and  is  therefore  used  as  the  negative 
pole  of  most  batteries ;  it  is  only  on  connecting  with  some 
less  electropositive  metal  that  hydrogen  is  evolved  from  the 
latter,  while  the  zinc  dissolves. 

"  Aluminium  bronze  "  is  an  alloy  of  aluminium  with 
copper,  containing  from  2  to  1 1  per  cent,  of  the  former 
metal.  It  resembles  gold  in  colour,  and  is  employed  in  the 
manufacture  of  imitation  jewellery. 

"  Ferro chrome  "  and  "  ferromanganese  "  are  produced 
by  simultaneous  reduction  of  ores  of  iron  and  chromium,  or 
of  iron  and  manganese.  Their  addition  in  small  quantity  to 
iron  improves  its  quality.  Iron  containing  about  i  o  per  cent, 
of  manganese  is  known  as  "  spiegel  iron,"  for  it  crystallises 
in  large  brilliant  plates.  Tungsten,  too,  is  sometimes  added 
to  iron  to  increase  its  hardness. 

"  Pewter"  is  an  alloy  of  80  per  cent,  of  lead  with  20  per 
cent,  of  tin ;  plumbers'  solder  consists  of  two  parts  of  lead 
to  one  of  tin ;  "  Britannia  metal "  is  made  of  equal  parts 
of  brass,  tin,  antimony,  and  bismuth. 

"  Bronze  "  is  one  of  the  most  ancient  alloys,  and  used  to 
be  made  by  reducing  together  copper  ores  and  tin  ores.  It 
often  contains  twenty-two  parts  of  tin  and  seventy-eight 
parts  of  copper.  Its  hardness  is  greatly  increased  by  the 
presence  of  a  trace  of  phosphorus.  "  Speculum  metal," 
for  astronomical  mirrors,  is  made  by  alloying  thirty-two 
parts  of  tin  with  sixty-seven  of  copper  and  one  of  arsenic. 
It  takes  a  very  high  polish.  Copper  is  easily  tinned  by 
melting  the  tin  in  the  vessel,  and  pouring  out  the  excess ; 
this  is  frequently  done  to  vessels  required  for  cooking. 

"Type-metal"  is  an  alloy  of  lead  and  antimony,  con- 
taining 1 8  per  cent  of  the  latter.  It  expands  slightly  on 
solidifying,  and  consequently  when  cast  in  the  mould  it  takes 
an  accurate  impression  and  forms  a  clean-cut  type. 

The  "Pattinson's  process"  is  a  rival  of  the  Parke's 
process  in  desilverising  crude  lead.  The  lead  is  melted  and 
allowed  to  solidify  partially ;  the  solid  portion  consists  of 


ALLOYS  197 

nearly  pure  lead.  The  liquid  portion  contains  the  silver. 
By  repetition  of  the  process,  the  lead  may  be  nearly  com- 
pletely deprived  of  silver ;  and  an  alloy  rich  in  silver  may 
be  obtained,  from  which  the  lead  may  be  removed  by 
cupellation. 

Osmiridium  is  a  native  alloy  of  osmium  and  iridium  ;  it 
is  extremely  hard,  and  it  is  used  for  pointing  gold  pens  and 
for  the  bearings  of  small  wheels.  An  alloy  of  platinum 
with  10  per  cent,  of  iridium  is  the  metal  employed  for 
crucibles. 

An  alloy  of  copper  and  silver  is  used  for  coinage  ; 
English  coins  contain  7.5  per  cent,  of  copper.  The  alloy 
must  be  rapidly  cooled,  else  it  ceases  to  be  homogeneous. 
Gold  is  also  alloyed  with  copper  for  coinage ;  pure  gold  is 
a  soft  metal.  The  English  standard  is  eleven  parts  of  gold 
to  one  of  copper ;  in  France  and  the  United  States,  nine  of 
gold  to  one  of  copper.  The  richness  of  such  an  alloy  is 
measured  in  "carats."  Pure  gold  is  "  24-carat  gold;" 
"  i8-carat  gold"  contains  eighteen  parts  of  gold  and  six  of 
copper. 

The  study  of  the  chemistry  of  metallic  alloys  was  for 
long  neglected,  but  of  recent  years  much  has  been  done. 
It  is  curious  to  think  that  the  successful  solution  of  many 
chemical  problems  is  to  be  expected  from  careful  examina- 
tion of  this  class  of  substances,  which  was  the  first  to  engage 
the  attention  of  the  chemists  of  the  remote  past. 


INDEX 


ACETIC  acid,  112 
Acetylene,  32,  36 
Acid  chlorides,  123 
Acids,  40,  69 

,,     rneta,  124 

,,     ortho,  123 

,,     pyro,  125 
Air,  2 

,,   analysis  of,  4 
,,    liquid,  26 
Alcohols,  67,  87,  88 
Aldehydes,  88 
Alloys,  191 

,,      fusible,  194 
Aluminates,  78 
Aluminium,  9,  16 

,,          hydroxide,  77 
Amalgams,  194 
Amines,  89,  171 

,,       salts  of,  177 
Ammonia,  32,  36,  37,  42 
Ammonium  halides,  65,  66 
,,  hydroxide,  86 

Antimonides,  181 
Antimony,  16 

,,         hydride,  38 
Argentamines,  180 
Argentocyanides,  178 
Argon,  5 
Arsenates,  129 
Arsenic,  16,  17 

, ,       hydride,  38 
Arsenides,  181 
Arsenites,  136 
Atmosphere,  2 
Auramines,  180 


199 


Auric  chloride,  56 
Aurocyanides,  187 

BARIUM,  8,  16 

,,         dioxide,  92 
,,         oxide,  77 
Basic  oxides,  76 

,,     salts,  104 
Basicity,  125 
Bauxite,  6 
Benzene,  49 
Beryllium,  8,  16 
Bismuth,  16 

,,        hydroxide,  77 
Biuret,  175 

Bleaching-powder,  141 
Borates,  105 
Borides,  189 
Boron,  16,  17 

,,      fluoride,  59 

,,      hydride,  38 
Brass,  195 
Brin's  process,  13 
Bromates,  144 
Bromine,  u,  15,  23 

,,        hydride,  34,  41 
Bronze,  196 

CADMIUM,  17 

,,         hydroxide,  77 
Caesium,  8 

,,         hydroxide,  74 
Calcium,  8,  16 

,,        oxide,  76 
Carbamates,  173 


INDEX 


Carbamine,  174 
Carbides,  36,  190 
Carbon,  acids  of,  112 

,,        chloride,  58 

,,        gas-,  12 

,,        hydrides,  32 

,,        monoxide,  93 

,,        oxysulphide,  in 
Carbonates,  106 

,,          acid,  109 
,,          basic,  108 
,,          native,  108 
Carborundum,  191 
Cerium,  16 

Chemical  action,  rate  of,  34 
Chlorates,  142 
Chloride  of  lime,  141 
Chlorine,  n,  15,  21 

,,        hydride,  34,  41 

,,        monoxide,  141 

,,       peroxide,  143 
Chlorochromates,  150 
Chlorosulphonic  acid,  150 
Chromamines,  178 
Chromates,  151 
Chromic  acid,  152 
Chromicyanides,  187 
Chromium  halides,  63 

,,          hydroxides,  77,  78 
Chromyl  chloride,  150 
Classification,  30 
Coal-gas,  12 
Cobalt,  16,  18 

,,     amines,  178 

,,     halides,  63 

,,     hydroxide,  78 
Coinage,  197 

Complex  groups,  oxides  of,  86 
Complexity,  molecular,  45,  99 
Compounds,  i,  30 
Copper,  9,  16,  18,  23 

,,       hydroxide,  77,  78 
Cupramines,  179 
Cupric  iodide,  56 
Cupricyanides,  188 
Cuprous  chloride,  54 
Cyanides,  182,  183 


DISPLACEMENT,  15 


ELECTRIC  potential,  23 
Electrolysis,  7 
Elements,  6 

,,         properties   of,   26,  27, 
28,  29 

,,        separation  of,  7 
Ethers,  90 
Ethylene,  36 

FERRICYANIDES,  185 
Ferrochrome,  196 
Ferrocyanides,  185 
Ferromanganese,  196 
Fluorine,  n 

,,        hydride,  33,  40 
Flux,  16 
Formic  acid,  112 


GALLIUM,  9 

,,         hydroxide,  77 
Galvanised  iron,  195 
Gases,  solution  of,  3 
German  silver,  195 
Germanium,  16,  18 

,,  hydroxide,  77 

Gold,  10,  12,  23 
Graham's  Law,  3 
Guanidine,  172 


HALIDES,  50 

,,        double,  54 
Halogens,  hydrides  of,  33 
Helium,  4 
Hydrazine,  42,  86 
Hydrazoates,  170 
Hydrazoic  acid,  41 
Hydrides,  30 
Hydrocarbons,  45 
Hydrocyanic  acid,  182 
Hydrogen,  12,  24 

bromide,  34,  35,  37 
chloride,  34,  35,  37 

,,         dioxide,  92 

,,         fluoride,  33,  35 
iodide,  3^  37 

,,         liquid,  6 
Hydrolysis,  51,  53 


INDEX 


Hydrosulphides,  69,  81,  82,  83 
Hydrosulphites,  166 
Hydroxides,  69,  71,  72,  73,  74 

,,          properties  of,  78 
Hydroxylamine,  87 
Hypobromites,  144- 
Hypochlorites,  140 
Hypoiodites,  134 
Hyponitrites,  138 
Hypophosphates,  137 
Hypophosphites,  136 

INACTIVE  gases,  4 
Indicators,  75 
Indium,  16,  17 

,,       hydroxide,  77 
"Insoluble"  substances,  70 
lodates,  134 
Iodine,  n,  15,  23 
,,      halides  of,  60 
,,      hydride,  34 
lodometry,  165 
lodonium  compounds,  91 
Ions,  colour  of,  64 
Iridium,  12 
Iron,  16,  18,  19 

,,   halides,  63 

,,    hydride,  31 

,,    hydroxides,  78 

KRYPTON,  5 

LANTHANUM,  16 

,,  hydroxide,  77 

Lead,  16,  18,  25 
,,     chlorides,  62 
,,     hydroxide,  77 
Lithium,  8,  n 
,,       hydride,  31 
,,       hydroxide,  74 

MAGNESIUM,  8,  16 

,,  hydroxide,  77 

Manganates,  152 
Manganese,  18 

,,          dioxide,  102 
,,          halides,  63 

hydroxides,  78 
Manganicyanides,  187 


Marsh's  test,  39 
Mass-action,  14,  62 
Mercuramines,  180 
Mercuric  iodide,  56 
Mercury,  12,  22 
Meteoric  iron,  31 
Methane,  32,  36 
Mixtures,  I 
Molybdates,  154 
Molybdenum  halides,  63 


NASCENT  state,  39,  42 
Neon,  5 

Neutral  oxides,  98 
Neutralisation,  75 
Nickel,  10,  16,  18 
,,      halides,  63 
,,      hydride,  31 
,,      hydroxide,  78,  79 
Niobium,  16 
Nitrates,  127 

Nitric  acid,  action  on  metals,  95 
,,         ,,      oxidation  with,  97 
,,      oxide,  97 
,,      peroxide,  98 
Nitrides,  37,  169 
Nitrites,  134 
Nitrogen,  22 

,,         iodide,  59 

,,         oxygen  compounds  of, 

132 

,,         chloride,  58 
Nitrous  oxide,  95 


OSMIRIDIUM,  197 

Osmium,  12 
Osmocyanides,  187 
Osmosis,  116 
Oxalic  acid,  113 
Oxidation,  64 
Oxides,  69 

,,      formation  of,  80,  81 
Oxygen,  13,  15 
Ozone,  23 


PALLADIUM,  12 

,,          halides,  64 


INDEX 


Palladium  hydride,  31 
Parke's  process,  195 
Pattison's  process,  196 
Perborates,  168 
Percarbonates,  168 
Perchlorates,  142 
Perchromic  acid,  167 
Periodates,  134 
Permanganates,  152 
Peroxides,  192 
Persulphates,  168 
Pewter,  196 
Phosphamides,  176 
Phosphates,  126 
Phosphides,  37,  181 
Phosphines,  89 
Phosphonium  halides,  65,  66 
Phosphorus,  18 

,,  acids,  133 

,,  halides,  64 

,,  hydride,  36,  37 

Platinum,  12 

,,         halides,  64 

,,         hydride,  31 
Polymerisation,  48 
Potassium,  8,  17 

,,          hydroxide,  74 

,,          tetroxide,  92 
Potential,  electric,  23 


REDUCTION,  25,  64 
Rhodium,  12 
Rubidium,  8,  17 

,,          hydroxide,  74 
Ruthenium,  12 
Ruthenocyanides,  187 


SCANDIUM,  16,  25 

,,  hydroxide,  77 

Selenates,  159 

Selenic  acids,  159 

Selenides,  69 

Selenious  acid,  146,  149 

Selenium,  12,  22 

,,        halides,  60 
,,       hydride,  39 

Silicates,  115 

Silicides,  191 


Silicon,  16,  17 

,,       fluoride,  59 
Silver,  ID,  12,  16,  23 

,,     hydroxide,  77,  78 

,,     oxide,  79 
Sodium,  8,  17,  18 

,,        dioxide,  92 

,,        hydride,  31 

,,       hydroxide,  74 
Solder,  196 

Solubility-product,  83,  84,  85 
Solution  of  gases,  3 
Spinels,  100 
Steel,  21 
Strontium,  8,  16 

„         oxide,  76 
Sulphamides,  177 
Sulphates,  159 
Sulphides,  69,  81 
Sulphites,  147,  148 
Sulphonates,  148 
Sulphur,  12,  22 

,,       ethers,  90 

,,        halides,  60 

hydride,  33,  39 

,,        trioxide,  155 
Sulphuric  acid,  155 
Sulphurous  acid,  146,  149 
Sulphuryl  chloride,  149 


TANTALUM,  16 
Tellurates,  159 
Telluric  acid,  159 
Tellurides,  69 
Tellurium,  12,  22 

,,         halides,  60 

,,         hydride,  39 
Tellurous  acid,  149 
Thallium,  16,  18 

,,        hydroxide,  77 
Thermal  data,  145 
Thio-acids,  130 
Thiocarbonates,  106,  no 
Thionates,  166 
Thiosulphates,  164 
Thorium,  16 

,,        hydroxide,  77 
Tin,  16,  18,  24, 
,,    chlorides,  62 


INDEX 


203 


Tin,  hydroxides,  77 
Tinned  iron,  195 
Titanium,  16,  17 

,,       hydroxide,  77 
Tungstates,  154 
Tungsten  halides,  63 
Type-metal,  196 

URANATES,  154 
Uranium  halides,  63 
Urea,  174 

VALENCY,  61 
Vanadates,  129 
Vanadium,  16 


WATER,  32,  35,  36 

,,       of  crystallisation,  53 


XENON,  5 

YTTERBIUM,  16 
Yttrium,  17 

,,       hydroxide,  77 

ZINC,  17,  19 

,,     hydroxide,  77 
Zincates,  78 
Zirconium  hydroxide,  77 


THE    END 


Printed  by  BALLANTYNE,   HANSON  < 
Edinburgh  &*  London 


Co. 


UNIVERSITY  OF  CALIFORNIA  LIBRARY, 
BERKELEY 


THIS  BOOK  IS  DUE  ON  THE  LAST  DATE 
STAMPED  BELOW 

Books  not  returned  on  time  are  subject  to  a  fine  of 
50c  per  volume  after  the  third  day  overdue,  increasing 
to  $1.00  per  volume  after  the  sixth  day.  Books  not  in 
demand  may  be  renewed  if  application  is  made  before 
expiration  of  loan  period. 


FEB   28  1943 


YA  02*81 


285213 


UNIVERSITY  OF  CALIFORNIA  LIBRARY